Articles | Volume 13, issue 12
https://doi.org/10.5194/se-13-1859-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/se-13-1859-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Review article
| 
16 Dec 2022
Review article |
| 16 Dec 2022
Analogue modelling of basin inversion: a review and future perspectives
Institute of Geological Sciences, University of Bern, Bern,
Switzerland
Helmholtz Centre Potsdam, German Research Centre for Geosciences
(GFZ), Potsdam, Germany
Guido Schreurs
Institute of Geological Sciences, University of Bern, Bern,
Switzerland
Susanne J. H. Buiter
Helmholtz Centre Potsdam, German Research Centre for Geosciences
(GFZ), Potsdam, Germany
Tectonics and Geodynamics, Faculty of Georesources and Materials
Engineering, RWTH Aachen University, Aachen, Germany
Oriol Ferrer
Geomodels Research
Institute, Departament de Dinàmica de la Terra i de l'Oceà, Facultat de Ciències de la Terra, Universitat de Barcelona, Barcelona, Spain
Riccardo Reitano
Department of Geological
Sciences, Università Degli Studi Roma Tre, Rome, Italy
Michael Rudolf
Helmholtz Centre Potsdam, German Research Centre for Geosciences
(GFZ), Potsdam, Germany
Engineering Geology Research Group, Institute for Applied Geosciences,
Technical University Darmstadt, Darmstadt, Germany
Ernst Willingshofer
Department of Earth Sciences, Utrecht University, Utrecht, the
Netherlands
Related authors
Frank Zwaan and Guido Schreurs
Solid Earth, 14, 823–845, https://doi.org/10.5194/se-14-823-2023, https://doi.org/10.5194/se-14-823-2023, 2023
Short summary
Short summary
The East African Rift System (EARS) is a major plate tectonic feature splitting the African continent apart. Understanding the tectonic processes involved is of great importance for societal and economic reasons (natural hazards, resources). Laboratory experiments allow us to simulate these large-scale processes, highlighting the links between rotational plate motion and the overall development of the EARS. These insights are relevant when studying other rift systems around the globe as well.
This article is included in the Encyclopedia of Geosciences
Pâmela Cristina Richetti, Frank Zwaan, Guido Schreurs, Renata S. Schmitt, and Timothy Chris Schmid
EGUsphere, https://doi.org/10.5194/egusphere-2022-1251, https://doi.org/10.5194/egusphere-2022-1251, 2022
Short summary
Short summary
The Araripe Basin in NE Brazil was originally formed during Cretaceous times, as South America and Africa broke up. The basin is an important analogue to offshore South Atlantic break-up basins; its sediments were uplifted and are now found at a 1000 m height, allowing for study, but the cause of the uplift remains debated. Here we ran a series of tectonic laboratory experiments that show how a specific plate tectonic configuration can explain the evolution of the Araripe Basin.
This article is included in the Encyclopedia of Geosciences
Frank Zwaan, Pauline Chenin, Duncan Erratt, Gianreto Manatschal, and Guido Schreurs
Solid Earth, 12, 1473–1495, https://doi.org/10.5194/se-12-1473-2021, https://doi.org/10.5194/se-12-1473-2021, 2021
Short summary
Short summary
We used laboratory experiments to simulate the early evolution of rift systems, and the influence of structural weaknesses left over from previous tectonic events that can localize new deformation. We find that the orientation and type of such weaknesses can induce complex structures with different orientations during a single phase of rifting, instead of requiring multiple rifting phases. These findings provide a strong incentive to reassess the tectonic history of various natural examples.
This article is included in the Encyclopedia of Geosciences
Frank Zwaan, Guido Schreurs, and Susanne J. H. Buiter
Solid Earth, 10, 1063–1097, https://doi.org/10.5194/se-10-1063-2019, https://doi.org/10.5194/se-10-1063-2019, 2019
Short summary
Short summary
This work was inspired by an effort to numerically reproduce laboratory models of extension tectonics. We tested various set-ups to find a suitable analogue model and in the process systematically charted the impact of set-ups and boundary conditions on model results, a topic poorly described in existing scientific literature. We hope that our model results and the discussion on which specific tectonic settings they could represent may serve as a guide for future (analogue) modeling studies.
This article is included in the Encyclopedia of Geosciences
Roy Helge Gabrielsen, Panagiotis Athanasios Giannenas, Dimitrios Sokoutis, Ernst Willingshofer, Muhammad Hassaan, and Jan Inge Faleide
Solid Earth, 14, 961–983, https://doi.org/10.5194/se-14-961-2023, https://doi.org/10.5194/se-14-961-2023, 2023
Short summary
Short summary
The Barents Shear Margin defines the border between the relatively shallow Barents Sea that is situated on a continental plate and the deep ocean. This margin's evolution history was probably influenced by plate tectonic reorganizations. From scaled experiments, we deduced several types of structures (faults, folds, and sedimentary basins) that help us to improve the understanding of the history of the opening of the North Atlantic.
This article is included in the Encyclopedia of Geosciences
Frank Zwaan and Guido Schreurs
Solid Earth, 14, 823–845, https://doi.org/10.5194/se-14-823-2023, https://doi.org/10.5194/se-14-823-2023, 2023
Short summary
Short summary
The East African Rift System (EARS) is a major plate tectonic feature splitting the African continent apart. Understanding the tectonic processes involved is of great importance for societal and economic reasons (natural hazards, resources). Laboratory experiments allow us to simulate these large-scale processes, highlighting the links between rotational plate motion and the overall development of the EARS. These insights are relevant when studying other rift systems around the globe as well.
This article is included in the Encyclopedia of Geosciences
Riccardo Reitano, Romano Clementucci, Ethan M. Conrad, Fabio Corbi, Riccardo Lanari, Claudio Faccenna, and Chiara Bazzucchi
Earth Surf. Dynam., 11, 731–740, https://doi.org/10.5194/esurf-11-731-2023, https://doi.org/10.5194/esurf-11-731-2023, 2023
Short summary
Short summary
Tectonics and surface processes work together in shaping orogens through their evolution. Laboratory models are used to overcome some limitations of direct observations since they allow for continuous and detailed analysis of analog orogens. We use a rectangular box filled with an analog material made of granular materials to study how erosional laws apply and how erosion affects the analog landscape as a function of the applied boundary conditions (regional slope and rainfall rate).
This article is included in the Encyclopedia of Geosciences
Natalie Hummel, Susanne Buiter, and Zoltán Erdös
EGUsphere, https://doi.org/10.5194/egusphere-2023-1656, https://doi.org/10.5194/egusphere-2023-1656, 2023
Short summary
Short summary
Simulations of subducting tectonic plates often use material properties extrapolated from the behavior of small rock samples in a laboratory to conditions found in the Earth. We explore several typical approaches to simulating these extrapolated material properties and show that they produce very rigid subducting plates with unrealistic dynamics. Our findings imply that subducting plates deform by additional mechanisms that are less commonly implemented in simulations.
This article is included in the Encyclopedia of Geosciences
Elizabeth Parker Wilson, Pablo Granado, Pablo Santolaria, Oriol Ferrer, and Josep Anton Muñoz
Solid Earth, 14, 709–739, https://doi.org/10.5194/se-14-709-2023, https://doi.org/10.5194/se-14-709-2023, 2023
Short summary
Short summary
This work focuses on the control of accommodation zones on extensional and subsequent inversion in salt-detached domains using sandbox analogue models. During extension, the transfer zone acts as a pathway for the movement of salt, changing the expected geometries. When inverted, the salt layer and syn-inversion sedimentation control the deformation style in the salt-detached cover system. Three natural cases are compared to the model results and show similar inversion geometries.
This article is included in the Encyclopedia of Geosciences
Anna-Katharina Sieberer, Ernst Willingshofer, Thomas Klotz, Hugo Ortner, and Hannah Pomella
Solid Earth, 14, 647–681, https://doi.org/10.5194/se-14-647-2023, https://doi.org/10.5194/se-14-647-2023, 2023
Short summary
Short summary
Through analogue models and field observations, we investigate how inherited platform–basin geometries control strain localisation, style, and orientation of reactivated and new structures during inversion. Our study shows that the style of evolving thrusts and their changes along-strike are controlled by pre-existing rheological discontinuities. The results of this study are relevant for understanding inversion structures in general and for the European eastern Southern Alps in particular.
This article is included in the Encyclopedia of Geosciences
Oriol Ferrer, Eloi Carola, and Ken McClay
Solid Earth, 14, 571–589, https://doi.org/10.5194/se-14-571-2023, https://doi.org/10.5194/se-14-571-2023, 2023
Short summary
Short summary
Using an experimental approach based on scaled sandbox models, this work aims to understand how salt above different rotational fault blocks influences the cover geometry and evolution, first during extension and then during inversion. The results show that inherited salt structures constrain contractional deformation. We show for the first time how welds and fault welds are reopened during contractional deformation, having direct implications for the subsurface exploration of natural resources.
This article is included in the Encyclopedia of Geosciences
Jordi Miró, Oriol Ferrer, Josep Anton Muñoz, and Gianreto Manastchal
Solid Earth, 14, 425–445, https://doi.org/10.5194/se-14-425-2023, https://doi.org/10.5194/se-14-425-2023, 2023
Short summary
Short summary
Using the Asturian–Basque–Cantabrian system and analogue (sandbox) models, this work focuses on the linkage between basement-controlled and salt-decoupled domains and how deformation is accommodated between the two during extension and subsequent inversion. Analogue models show significant structural variability in the transitional domain, with oblique structures that can be strongly modified by syn-contractional sedimentation. Experimental results are consistent with the case study.
This article is included in the Encyclopedia of Geosciences
Timothy Chris Schmid, Sascha Brune, Anne Glerum, and Guido Schreurs
Solid Earth, 14, 389–407, https://doi.org/10.5194/se-14-389-2023, https://doi.org/10.5194/se-14-389-2023, 2023
Short summary
Short summary
Continental rifts form by linkage of individual rift segments and disturb the regional stress field. We use analog and numerical models of such rift segment interactions to investigate the linkage of deformation and stresses and subsequent stress deflections from the regional stress pattern. This local stress re-orientation eventually causes rift deflection when multiple rift segments compete for linkage with opposingly propagating segments and may explain rift deflection as observed in nature.
This article is included in the Encyclopedia of Geosciences
Denise Degen, Daniel Caviedes Voullième, Susanne Buiter, Harrie-Jan Hendriks Franssen, Harry Vereecken, Ana González-Nicolás, and Florian Wellmann
Geosci. Model Dev. Discuss., https://doi.org/10.5194/gmd-2022-309, https://doi.org/10.5194/gmd-2022-309, 2023
Revised manuscript under review for GMD
Short summary
Short summary
In geosciences, we often use simulations based on physical laws. These simulations can be computationally expensive, which is a problem if simulations must be performed many times (e.g., to add error bounds). We show how a novel machine learning method helps to reduce simulation time. In comparison to other approaches, which typically only look at the output of a simulation, the method considers physical laws in the simulation itself. The method provides reliable results faster than standard.
This article is included in the Encyclopedia of Geosciences
Michael Rudolf, Matthias Rosenau, and Onno Oncken
Solid Earth, 14, 311–331, https://doi.org/10.5194/se-14-311-2023, https://doi.org/10.5194/se-14-311-2023, 2023
Short summary
Short summary
Analogue models of tectonic processes rely on the reproduction of their geometry, kinematics and dynamics. An important property is fault behaviour, which is linked to the frictional characteristics of the fault gouge. This is represented by granular materials, such as quartz sand. In our study we investigate the time-dependent frictional properties of various analogue materials and highlight their impact on the suitability of these materials for analogue models focusing on fault reactivation.
This article is included in the Encyclopedia of Geosciences
Nicolás Molnar and Susanne Buiter
Solid Earth, 14, 213–235, https://doi.org/10.5194/se-14-213-2023, https://doi.org/10.5194/se-14-213-2023, 2023
Short summary
Short summary
Progression of orogenic wedges over pre-existing extensional structures is common in nature, but deciphering the spatio-temporal evolution of deformation from the geological record remains challenging. Our laboratory experiments provide insights on how horizontal stresses are transferred across a heterogeneous crust, constrain which pre-shortening conditions can either favour or hinder the reactivatation of extensional structures, and explain what implications they have on critical taper theory.
This article is included in the Encyclopedia of Geosciences
Willemijn S. M. T. van Kooten, Hugo Ortner, Ernst Willingshofer, Dimitrios Sokoutis, Alfred Gruber, and Thomas Sausgruber
EGUsphere, https://doi.org/10.5194/egusphere-2022-1529, https://doi.org/10.5194/egusphere-2022-1529, 2023
Short summary
Short summary
Extensional deformation creates structures that may be reactivated during subsequent shortening. The Achental structure within the Northern Calcareous Alps fold-and-thrust belt is a natural example of a basin margin that was inverted during Alpine orogeny. Based on this example, we have studied the influence of such inherited inhomogeneities in-field and as analogue model. We find that oblique shortening can create structures outlining pre-existing faults within a single deformation event.
This article is included in the Encyclopedia of Geosciences
Pâmela Cristina Richetti, Frank Zwaan, Guido Schreurs, Renata S. Schmitt, and Timothy Chris Schmid
EGUsphere, https://doi.org/10.5194/egusphere-2022-1251, https://doi.org/10.5194/egusphere-2022-1251, 2022
Short summary
Short summary
The Araripe Basin in NE Brazil was originally formed during Cretaceous times, as South America and Africa broke up. The basin is an important analogue to offshore South Atlantic break-up basins; its sediments were uplifted and are now found at a 1000 m height, allowing for study, but the cause of the uplift remains debated. Here we ran a series of tectonic laboratory experiments that show how a specific plate tectonic configuration can explain the evolution of the Araripe Basin.
This article is included in the Encyclopedia of Geosciences
Susanne J. H. Buiter, Sascha Brune, Derek Keir, and Gwenn Peron-Pinvidic
EGUsphere, https://doi.org/10.5194/egusphere-2022-139, https://doi.org/10.5194/egusphere-2022-139, 2022
Preprint archived
Short summary
Short summary
Continental rifts can form when and where continents are stretched. Rifts are characterised by faults, sedimentary basins, earthquakes and/or volcanism. If rifting can continue, a rift may break a continent into conjugate margins such as along the Atlantic and Indian Oceans. In some cases, however, rifting fails, such as in the West African Rift. We discuss continental rifting from inception to break-up, focussing on the processes at play, and illustrate these with several natural examples.
This article is included in the Encyclopedia of Geosciences
Hazel Gibson, Sam Illingworth, and Susanne Buiter
Geosci. Commun., 4, 437–451, https://doi.org/10.5194/gc-4-437-2021, https://doi.org/10.5194/gc-4-437-2021, 2021
Short summary
Short summary
In the spring of 2020, in response to the escalating global COVID-19 Coronavirus pandemic, the European Geosciences Union (EGU) moved its annual General Assembly online in a matter of weeks. This paper explores the feedback provided by participants who attended this experimental conference and identifies four key themes that emerged from analysis of the survey (connection, engagement, environment, and accessibility). The responses raise important questions about the format of future conferences.
This article is included in the Encyclopedia of Geosciences
Frank Zwaan, Pauline Chenin, Duncan Erratt, Gianreto Manatschal, and Guido Schreurs
Solid Earth, 12, 1473–1495, https://doi.org/10.5194/se-12-1473-2021, https://doi.org/10.5194/se-12-1473-2021, 2021
Short summary
Short summary
We used laboratory experiments to simulate the early evolution of rift systems, and the influence of structural weaknesses left over from previous tectonic events that can localize new deformation. We find that the orientation and type of such weaknesses can induce complex structures with different orientations during a single phase of rifting, instead of requiring multiple rifting phases. These findings provide a strong incentive to reassess the tectonic history of various natural examples.
This article is included in the Encyclopedia of Geosciences
Øystein T. Haug, Matthias Rosenau, Michael Rudolf, Karen Leever, and Onno Oncken
Earth Surf. Dynam., 9, 665–672, https://doi.org/10.5194/esurf-9-665-2021, https://doi.org/10.5194/esurf-9-665-2021, 2021
Short summary
Short summary
The runout of rock avalanches scales with their volume but also shows a considerable variation for avalanches with similar volumes. Here we show that besides size-dependent weakening mechanisms, fragmentation can account for the observed variability in runout. We use laboratory-scale experimental avalanches to simulate and analyse the role of fragmentation. We find that fragmentation consumes energy but also increases avalanche mobility. It does so systematically and predictably.
This article is included in the Encyclopedia of Geosciences
Riccardo Reitano, Claudio Faccenna, Francesca Funiciello, Fabio Corbi, and Sean D. Willett
Earth Surf. Dynam., 8, 973–993, https://doi.org/10.5194/esurf-8-973-2020, https://doi.org/10.5194/esurf-8-973-2020, 2020
Short summary
Short summary
Looking into processes that occur on different timescales that span over thousands or millions of years is difficult to achieve. This is the case when we try to understand the interaction between tectonics and surface processes. Analog modeling is an investigating technique that can overcome this limitation. We study the erosional response of an analog landscape by varying the concentration of components of analog materials that strongly affect the evolution of experimental landscapes.
This article is included in the Encyclopedia of Geosciences
Juan Alcalde, Clare E. Bond, Gareth Johnson, Armelle Kloppenburg, Oriol Ferrer, Rebecca Bell, and Puy Ayarza
Solid Earth, 10, 1651–1662, https://doi.org/10.5194/se-10-1651-2019, https://doi.org/10.5194/se-10-1651-2019, 2019
Carla Patricia Bárbara, Patricia Cabello, Alexandre Bouche, Ingrid Aarnes, Carlos Gordillo, Oriol Ferrer, Maria Roma, and Pau Arbués
Solid Earth, 10, 1597–1619, https://doi.org/10.5194/se-10-1597-2019, https://doi.org/10.5194/se-10-1597-2019, 2019
Frank Zwaan, Guido Schreurs, and Susanne J. H. Buiter
Solid Earth, 10, 1063–1097, https://doi.org/10.5194/se-10-1063-2019, https://doi.org/10.5194/se-10-1063-2019, 2019
Short summary
Short summary
This work was inspired by an effort to numerically reproduce laboratory models of extension tectonics. We tested various set-ups to find a suitable analogue model and in the process systematically charted the impact of set-ups and boundary conditions on model results, a topic poorly described in existing scientific literature. We hope that our model results and the discussion on which specific tectonic settings they could represent may serve as a guide for future (analogue) modeling studies.
This article is included in the Encyclopedia of Geosciences
J. L. Tetreault and S. J. H. Buiter
Solid Earth, 5, 1243–1275, https://doi.org/10.5194/se-5-1243-2014, https://doi.org/10.5194/se-5-1243-2014, 2014
Short summary
Short summary
Continents are composed of a collage of accreted terranes: tectonically sutured crustal units of various origins. This review covers the cycle of terrane accretion from the original entity (modern-day oceanic island arcs, oceanic plateaus, submarine ridges, seamounts, continental fragments, and microcontinents) to present-day examples of terrane accretion to finally allochthonous accreted terranes.
This article is included in the Encyclopedia of Geosciences
M. E. T. Quinquis and S. J. H. Buiter
Solid Earth, 5, 537–555, https://doi.org/10.5194/se-5-537-2014, https://doi.org/10.5194/se-5-537-2014, 2014
Related subject area
Subject area: Tectonic plate interactions, magma genesis, and lithosphere deformation at all scales | Editorial team: Structural geology and tectonics, paleoseismology, rock physics, experimental deformation | Discipline: Tectonics
Selective inversion of rift basins in lithospheric-scale analogue experiments
The link between Somalian Plate rotation and the East African Rift System: an analogue modelling study
Inversion of extensional basins parallel and oblique to their boundaries: inferences from analogue models and field observations from the Dolomites Indenter, European eastern Southern Alps
Magnetic fabric analyses of basin inversion: a sandbox modelling approach
The influence of crustal strength on rift geometry and development – insights from 3D numerical modelling
Construction of the Ukrainian Carpathian wedge from low-temperature thermochronology and tectono-stratigraphic analysis
Melt-enhanced strain localization and phase mixing in a large-scale mantle shear zone (Ronda peridotite, Spain)
Insights into the interaction of a shale with CO2
Tectonostratigraphic evolution of the Slyne Basin
Control of crustal strength, tectonic inheritance, and stretching/ shortening rates on crustal deformation and basin reactivation: insights from laboratory models
Late Cretaceous–early Palaeogene inversion-related tectonic structures at the northeastern margin of the Bohemian Massif (southwestern Poland and northern Czechia)
The analysis of slip tendency of major tectonic faults in Germany
Earthquake ruptures and topography of the Chilean margin controlled by plate interface deformation
Late Quaternary faulting in the southern Matese (Italy): implications for earthquake potential and slip rate variability in the southern Apennines
Rare earth elements associated with carbonatite–alkaline complexes in western Rajasthan, India: exploration targeting at regional scale
Structural complexities and tectonic barriers controlling recent seismic activity in the Pollino area (Calabria–Lucania, southern Italy) – constraints from stress inversion and 3D fault model building
The Mid Atlantic Appalachian Orogen Traverse: a comparison of virtual and on-location field-based capstone experiences
Chronology of thrust propagation from an updated tectono-sedimentary framework of the Miocene molasse (western Alps)
Orogenic lithosphere and slabs in the greater Alpine area – interpretations based on teleseismic P-wave tomography
Ground-penetrating radar signature of Quaternary faulting: a study from the Mt. Pollino region, southern Apennines, Italy
U–Pb dating of middle Eocene–Pliocene multiple tectonic pulses in the Alpine foreland
Detrital zircon provenance record of the Zagros mountain building from the Neotethys obduction to the Arabia–Eurasia collision, NW Zagros fold–thrust belt, Kurdistan region of Iraq
The Subhercynian Basin: an example of an intraplate foreland basin due to a broken plate
Late to post-Variscan basement segmentation and differential exhumation along the SW Bohemian Massif, central Europe
Holocene surface-rupturing earthquakes on the Dinaric Fault System, western Slovenia
Contribution of gravity gliding in salt-bearing rift basins – a new experimental setup for simulating salt tectonics under the influence of sub-salt extension and tilting
Thick- and thin-skinned basin inversion in the Danish Central Graben, North Sea – the role of deep evaporites and basement kinematics
Complex rift patterns, a result of interacting crustal and mantle weaknesses, or multiphase rifting? Insights from analogue models
Interactions of plutons and detachments: a comparison of Aegean and Tyrrhenian granitoids
Insights from elastic thermobarometry into exhumation of high-pressure metamorphic rocks from Syros, Greece
Stress rotation – impact and interaction of rock stiffness and faults
Late Cretaceous to Paleogene exhumation in central Europe – localized inversion vs. large-scale domal uplift
Kinematics and extent of the Piemont–Liguria Basin – implications for subduction processes in the Alps
Effects of basal drag on subduction dynamics from 2D numerical models
Hydrocarbon accumulation in basins with multiple phases of extension and inversion: examples from the Western Desert (Egypt) and the western Black Sea
Long-wavelength late-Miocene thrusting in the north Alpine foreland: implications for late orogenic processes
A reconstruction of Iberia accounting for Western Tethys–North Atlantic kinematics since the late-Permian–Triassic
The enigmatic curvature of Central Iberia and its puzzling kinematics
Control of 3-D tectonic inheritance on fold-and-thrust belts: insights from 3-D numerical models and application to the Helvetic nappe system
Plio-Quaternary tectonic evolution of the southern margin of the Alboran Basin (Western Mediterranean)
Surface deformation relating to the 2018 Lake Muir earthquake sequence, southwest Western Australia: new insight into stable continental region earthquakes
Seismic reflection data reveal the 3D structure of the newly discovered Exmouth Dyke Swarm, offshore NW Australia
Cenozoic deformation in the Tauern Window (Eastern Alps) constrained by in situ Th-Pb dating of fissure monazite
Uncertainties in break-up markers along the Iberia–Newfoundland margins illustrated by new seismic data
Tectonic inheritance controls nappe detachment, transport and stacking in the Helvetic nappe system, Switzerland: insights from thermomechanical simulations
Can subduction initiation at a transform fault be spontaneous?
The Geodynamic World Builder: a solution for complex initial conditions in numerical modeling
From mapped faults to fault-length earthquake magnitude (FLEM): a test on Italy with methodological implications
Lithosphere tearing along STEP faults and synkinematic formation of lherzolite and wehrlite in the shallow subcontinental mantle
A systematic comparison of experimental set-ups for modelling extensional tectonics
Anindita Samsu, Weronika Gorczyk, Timothy Chris Schmid, Peter Graham Betts, Alexander Ramsay Cruden, Eleanor Morton, and Fatemeh Amirpoorsaeed
Solid Earth, 14, 909–936, https://doi.org/10.5194/se-14-909-2023, https://doi.org/10.5194/se-14-909-2023, 2023
Short summary
Short summary
When a continent is pulled apart, it breaks and forms a series of depressions called rift basins. These basins lie above weakened crust that is then subject to intense deformation during subsequent tectonic compression. Our analogue experiments show that when a system of basins is squeezed in a direction perpendicular to the main trend of the basins, some basins rise up to form mountains while others do not.
This article is included in the Encyclopedia of Geosciences
Frank Zwaan and Guido Schreurs
Solid Earth, 14, 823–845, https://doi.org/10.5194/se-14-823-2023, https://doi.org/10.5194/se-14-823-2023, 2023
Short summary
Short summary
The East African Rift System (EARS) is a major plate tectonic feature splitting the African continent apart. Understanding the tectonic processes involved is of great importance for societal and economic reasons (natural hazards, resources). Laboratory experiments allow us to simulate these large-scale processes, highlighting the links between rotational plate motion and the overall development of the EARS. These insights are relevant when studying other rift systems around the globe as well.
This article is included in the Encyclopedia of Geosciences
Anna-Katharina Sieberer, Ernst Willingshofer, Thomas Klotz, Hugo Ortner, and Hannah Pomella
Solid Earth, 14, 647–681, https://doi.org/10.5194/se-14-647-2023, https://doi.org/10.5194/se-14-647-2023, 2023
Short summary
Short summary
Through analogue models and field observations, we investigate how inherited platform–basin geometries control strain localisation, style, and orientation of reactivated and new structures during inversion. Our study shows that the style of evolving thrusts and their changes along-strike are controlled by pre-existing rheological discontinuities. The results of this study are relevant for understanding inversion structures in general and for the European eastern Southern Alps in particular.
This article is included in the Encyclopedia of Geosciences
Thorben Schöfisch, Hemin Koyi, and Bjarne Almqvist
Solid Earth, 14, 447–461, https://doi.org/10.5194/se-14-447-2023, https://doi.org/10.5194/se-14-447-2023, 2023
Short summary
Short summary
A magnetic fabric analysis provides information about the reorientation of magnetic grains and is applied to three sandbox models that simulate different stages of basin inversion. The analysed magnetic fabrics reflect the different developed structures and provide insights into the different deformed stages of basin inversion. It is a first attempt of applying magnetic fabric analyses to basin inversion sandbox models but shows the possibility of applying it to such models.
This article is included in the Encyclopedia of Geosciences
Thomas B. Phillips, John B. Naliboff, Ken J. W. McCaffrey, Sophie Pan, Jeroen van Hunen, and Malte Froemchen
Solid Earth, 14, 369–388, https://doi.org/10.5194/se-14-369-2023, https://doi.org/10.5194/se-14-369-2023, 2023
Short summary
Short summary
Continental crust comprises bodies of varying strength, formed through numerous tectonic events. When subject to extension, these areas produce distinct rift and fault systems. We use 3D models to examine how rifts form above
This article is included in the Encyclopedia of Geosciences
strongand
weakareas of crust. We find that faults become more developed in weak areas. Faults are initially stopped at the boundaries with stronger areas before eventually breaking through. We relate our model observations to rift systems globally.
Marion Roger, Arjan de Leeuw, Peter van der Beek, Laurent Husson, Edward R. Sobel, Johannes Glodny, and Matthias Bernet
Solid Earth, 14, 153–179, https://doi.org/10.5194/se-14-153-2023, https://doi.org/10.5194/se-14-153-2023, 2023
Short summary
Short summary
We study the construction of the Ukrainian Carpathians with LT thermochronology (AFT, AHe, and ZHe) and stratigraphic analysis. QTQt thermal models are combined with burial diagrams to retrieve the timing and magnitude of sedimentary burial, tectonic burial, and subsequent exhumation of the wedge's nappes from 34 to ∼12 Ma. Out-of-sequence thrusting and sediment recycling during wedge building are also identified. This elucidates the evolution of a typical wedge in a roll-back subduction zone.
This article is included in the Encyclopedia of Geosciences
Sören Tholen, Jolien Linckens, and Gernold Zulauf
EGUsphere, https://doi.org/10.5194/egusphere-2022-1348, https://doi.org/10.5194/egusphere-2022-1348, 2023
Short summary
Short summary
Pre- to syn-deformational melts initiate shear localization in the km-scale shear zone of the northwestern Ronda peridotite. The crystallization of interstitial pyroxenes and melt-rock reactions at pyroxene porphyroclasts form a highly mixed assemblage (> 60 % phase boundaries). Strain localization in the melt-effected area is controlled by the activation of a grain-size-sensitive deformation mechanism under constant stress.
This article is included in the Encyclopedia of Geosciences
Eleni Stavropoulou and Lyesse Laloui
Solid Earth, 13, 1823–1841, https://doi.org/10.5194/se-13-1823-2022, https://doi.org/10.5194/se-13-1823-2022, 2022
Short summary
Short summary
Shales are identified as suitable caprock formations for geolocigal CO2 storage thanks to their low permeability. Here, small-sized shale samples are studied under field-representative conditions with X-ray tomography. The geochemical impact of CO2 on calcite-rich zones is for the first time visualised, the role of pre-existing micro-fissures in the CO2 invasion trapping in the matererial is highlighted, and the initiation of micro-cracks when in contact with anhydrous CO2 is demonstrated.
This article is included in the Encyclopedia of Geosciences
Conor M. O'Sullivan, Conrad J. Childs, Muhammad M. Saqab, John J. Walsh, and Patrick M. Shannon
Solid Earth, 13, 1649–1671, https://doi.org/10.5194/se-13-1649-2022, https://doi.org/10.5194/se-13-1649-2022, 2022
Short summary
Short summary
The Slyne Basin is a sedimentary basin located offshore north-western Ireland. It formed through a long and complex evolution involving distinct periods of extension. The basin is subdivided into smaller basins, separated by deep structures related to the ancient Caledonian mountain-building event. These deep structures influence the shape of the basin as it evolves in a relatively unique way, where early faults follow these deep structures, but later faults do not.
This article is included in the Encyclopedia of Geosciences
Benjamin Guillaume, Guido M. Gianni, Jean-Jacques Kermarrec, and Khaled Bock
Solid Earth, 13, 1393–1414, https://doi.org/10.5194/se-13-1393-2022, https://doi.org/10.5194/se-13-1393-2022, 2022
Short summary
Short summary
Under tectonic forces, the upper part of the crust can break along different types of faults, depending on the orientation of the applied stresses. Using scaled analogue models, we show that the relative magnitude of compressional and extensional forces as well as the presence of inherited structures resulting from previous stages of deformation control the location and type of faults. Our results gives insights into the tectonic evolution of areas showing complex patterns of deformation.
This article is included in the Encyclopedia of Geosciences
Andrzej Głuszyński and Paweł Aleksandrowski
Solid Earth, 13, 1219–1242, https://doi.org/10.5194/se-13-1219-2022, https://doi.org/10.5194/se-13-1219-2022, 2022
Short summary
Short summary
Old seismic data recently reprocessed with modern software allowed us to study at depth the Late Cretaceous tectonic structures in the Permo-Mesozoic rock sequences in the Sudetes. The structures formed in response to Iberia collision with continental Europe. The NE–SW compression undulated the crystalline basement top and produced folds, faults and joints in the sedimentary cover. Our results are of importance for regional geology and in prospecting for deep thermal waters.
This article is included in the Encyclopedia of Geosciences
Luisa Röckel, Steffen Ahlers, Birgit Müller, Karsten Reiter, Oliver Heidbach, Andreas Henk, Tobias Hergert, and Frank Schilling
Solid Earth, 13, 1087–1105, https://doi.org/10.5194/se-13-1087-2022, https://doi.org/10.5194/se-13-1087-2022, 2022
Short summary
Short summary
Reactivation of tectonic faults can lead to earthquakes and jeopardize underground operations. The reactivation potential is linked to fault properties and the tectonic stress field. We create 3D geometries for major faults in Germany and use stress data from a 3D geomechanical–numerical model to calculate their reactivation potential and compare it to seismic events. The reactivation potential in general is highest for NNE–SSW- and NW–SE-striking faults and strongly depends on the fault dip.
This article is included in the Encyclopedia of Geosciences
Nadaya Cubas, Philippe Agard, and Roxane Tissandier
Solid Earth, 13, 779–792, https://doi.org/10.5194/se-13-779-2022, https://doi.org/10.5194/se-13-779-2022, 2022
Short summary
Short summary
Earthquake extent prediction is limited by our poor understanding of slip deficit patterns. From a mechanical analysis applied along the Chilean margin, we show that earthquakes are bounded by extensive plate interface deformation. This deformation promotes stress build-up, leading to earthquake nucleation; earthquakes then propagate along smoothed fault planes and are stopped by heterogeneously distributed deformation. Slip deficit patterns reflect the spatial distribution of this deformation.
This article is included in the Encyclopedia of Geosciences
Paolo Boncio, Eugenio Auciello, Vincenzo Amato, Pietro Aucelli, Paola Petrosino, Anna C. Tangari, and Brian R. Jicha
Solid Earth, 13, 553–582, https://doi.org/10.5194/se-13-553-2022, https://doi.org/10.5194/se-13-553-2022, 2022
Short summary
Short summary
We studied the Gioia Sannitica normal fault (GF) within the southern Matese fault system (SMF) in southern Apennines (Italy). It is a fault with a long slip history that has experienced recent reactivation or acceleration. Present activity has resulted in late Quaternary fault scarps and Holocene surface faulting. The maximum slip rate is ~ 0.5 mm/yr. Activation of the 11.5 km GF or the entire 30 km SMF can produce up to M 6.2 or M 6.8 earthquakes, respectively.
This article is included in the Encyclopedia of Geosciences
Malcolm Aranha, Alok Porwal, Manikandan Sundaralingam, Ignacio González-Álvarez, Amber Markan, and Karunakar Rao
Solid Earth, 13, 497–518, https://doi.org/10.5194/se-13-497-2022, https://doi.org/10.5194/se-13-497-2022, 2022
Short summary
Short summary
Rare earth elements (REEs) are considered critical mineral resources for future industrial growth due to their short supply and rising demand. This study applied an artificial-intelligence-based technique to target potential REE-deposit hosting areas in western Rajasthan, India. Uncertainties associated with the prospective targets were also estimated to aid decision-making. The presented workflow can be applied to similar regions elsewhere to locate potential zones of REE mineralisation.
This article is included in the Encyclopedia of Geosciences
Daniele Cirillo, Cristina Totaro, Giusy Lavecchia, Barbara Orecchio, Rita de Nardis, Debora Presti, Federica Ferrarini, Simone Bello, and Francesco Brozzetti
Solid Earth, 13, 205–228, https://doi.org/10.5194/se-13-205-2022, https://doi.org/10.5194/se-13-205-2022, 2022
Short summary
Short summary
The Pollino region is a highly seismic area of Italy. Increasing the geological knowledge on areas like this contributes to reducing risk and saving lives. We reconstruct the 3D model of the faults which generated the 2010–2014 seismicity integrating geological and seismological data. Appropriate relationships based on the dimensions of the activated faults suggest that they did not fully discharge their seismic potential and could release further significant earthquakes in the near future.
This article is included in the Encyclopedia of Geosciences
Steven Whitmeyer, Lynn Fichter, Anita Marshall, and Hannah Liddle
Solid Earth, 12, 2803–2820, https://doi.org/10.5194/se-12-2803-2021, https://doi.org/10.5194/se-12-2803-2021, 2021
Short summary
Short summary
Field trips in the Stratigraphy, Structure, Tectonics (SST) course transitioned to a virtual format in Fall 2020, due to the COVID pandemic. Virtual field experiences (VFEs) were developed in web Google Earth and were evaluated in comparison with on-location field trips via an online survey. Students recognized the value of VFEs for revisiting outcrops and noted improved accessibility for students with disabilities. Potential benefits of hybrid field experiences were also indicated.
This article is included in the Encyclopedia of Geosciences
Amir Kalifi, Philippe Hervé Leloup, Philippe Sorrel, Albert Galy, François Demory, Vincenzo Spina, Bastien Huet, Frédéric Quillévéré, Frédéric Ricciardi, Daniel Michoux, Kilian Lecacheur, Romain Grime, Bernard Pittet, and Jean-Loup Rubino
Solid Earth, 12, 2735–2771, https://doi.org/10.5194/se-12-2735-2021, https://doi.org/10.5194/se-12-2735-2021, 2021
Short summary
Short summary
Molasse deposits, deposited and deformed at the western Alpine front during the Miocene (23 to 5.6 Ma), record the chronology of that deformation. We combine the first precise chronostratigraphy (precision of ∼0.5 Ma) of the Miocene molasse, the reappraisal of the regional structure, and the analysis of growth deformation structures in order to document three tectonic phases and the precise chronology of thrust westward propagation during the second one involving the Belledonne basal thrust.
This article is included in the Encyclopedia of Geosciences
Mark R. Handy, Stefan M. Schmid, Marcel Paffrath, Wolfgang Friederich, and the AlpArray Working Group
Solid Earth, 12, 2633–2669, https://doi.org/10.5194/se-12-2633-2021, https://doi.org/10.5194/se-12-2633-2021, 2021
Short summary
Short summary
New images from the multi-national AlpArray experiment illuminate the Alps from below. They indicate thick European mantle descending beneath the Alps and forming blobs that are mostly detached from the Alps above. In contrast, the Adriatic mantle in the Alps is much thinner. This difference helps explain the rugged mountains and the abundance of subducted and exhumed units at the core of the Alps. The blobs are stretched remnants of old ocean and its margins that reach down to at least 410 km.
This article is included in the Encyclopedia of Geosciences
Maurizio Ercoli, Daniele Cirillo, Cristina Pauselli, Harry M. Jol, and Francesco Brozzetti
Solid Earth, 12, 2573–2596, https://doi.org/10.5194/se-12-2573-2021, https://doi.org/10.5194/se-12-2573-2021, 2021
Short summary
Short summary
Past strong earthquakes can produce topographic deformations, often
This article is included in the Encyclopedia of Geosciences
memorizedin Quaternary sediments, which are typically studied by paleoseismologists through trenching. Using a ground-penetrating radar (GPR), we unveiled possible buried Quaternary faulting in the Mt. Pollino seismic gap region (southern Italy). We aim to contribute to seismic hazard assessment of an area potentially prone to destructive events as well as promote our workflow in similar contexts around the world.
Luca Smeraglia, Nathan Looser, Olivier Fabbri, Flavien Choulet, Marcel Guillong, and Stefano M. Bernasconi
Solid Earth, 12, 2539–2551, https://doi.org/10.5194/se-12-2539-2021, https://doi.org/10.5194/se-12-2539-2021, 2021
Short summary
Short summary
In this paper, we dated fault movements at geological timescales which uplifted the sedimentary successions of the Jura Mountains from below the sea level up to Earth's surface. To do so, we applied the novel technique of U–Pb geochronology on calcite mineralizations that precipitated on fault surfaces during times of tectonic activity. Our results document a time frame of the tectonic evolution of the Jura Mountains and provide new insight into the broad geological history of the Western Alps.
This article is included in the Encyclopedia of Geosciences
Renas I. Koshnaw, Fritz Schlunegger, and Daniel F. Stockli
Solid Earth, 12, 2479–2501, https://doi.org/10.5194/se-12-2479-2021, https://doi.org/10.5194/se-12-2479-2021, 2021
Short summary
Short summary
As continental plates collide, mountain belts grow. This study investigated the provenance of rocks from the northwestern segment of the Zagros mountain belt to unravel the convergence history of the Arabian and Eurasian plates. Provenance data synthesis and field relationships suggest that the Zagros Mountains developed as a result of the oceanic crust emplacement on the Arabian continental plate, followed by the Arabia–Eurasia collision and later uplift of the broader region.
This article is included in the Encyclopedia of Geosciences
David Hindle and Jonas Kley
Solid Earth, 12, 2425–2438, https://doi.org/10.5194/se-12-2425-2021, https://doi.org/10.5194/se-12-2425-2021, 2021
Short summary
Short summary
Central western Europe underwent a strange episode of lithospheric deformation, resulting in a chain of small mountains that run almost west–east across the continent and that formed in the middle of a tectonic plate, not at its edges as is usually expected. Associated with these mountains, in particular the Harz in central Germany, are marine basins contemporaneous with the mountain growth. We explain how those basins came to be as a result of the mountains bending the adjacent plate.
This article is included in the Encyclopedia of Geosciences
Andreas Eberts, Hamed Fazlikhani, Wolfgang Bauer, Harald Stollhofen, Helga de Wall, and Gerald Gabriel
Solid Earth, 12, 2277–2301, https://doi.org/10.5194/se-12-2277-2021, https://doi.org/10.5194/se-12-2277-2021, 2021
Short summary
Short summary
We combine gravity anomaly and topographic data with observations from thermochronology, metamorphic grades, and the granite inventory to detect patterns of basement block segmentation and differential exhumation along the southwestern Bohemian Massif. Based on our analyses, we introduce a previously unknown tectonic structure termed Cham Fault, which, together with the Pfahl and Danube shear zones, is responsible for the exposure of different crustal levels during late to post-Variscan times.
This article is included in the Encyclopedia of Geosciences
Christoph Grützner, Simone Aschenbrenner, Petra Jamšek
Rupnik, Klaus Reicherter, Nour Saifelislam, Blaž Vičič, Marko Vrabec, Julian Welte, and Kamil Ustaszewski
Solid Earth, 12, 2211–2234, https://doi.org/10.5194/se-12-2211-2021, https://doi.org/10.5194/se-12-2211-2021, 2021
Short summary
Short summary
Several large strike-slip faults in western Slovenia are known to be active, but most of them have not produced strong earthquakes in historical times. In this study we use geomorphology, near-surface geophysics, and fault excavations to show that two of these faults had surface-rupturing earthquakes during the Holocene. Instrumental and historical seismicity data do not capture the strongest events in this area.
This article is included in the Encyclopedia of Geosciences
Michael Warsitzka, Prokop Závada, Fabian Jähne-Klingberg, and Piotr Krzywiec
Solid Earth, 12, 1987–2020, https://doi.org/10.5194/se-12-1987-2021, https://doi.org/10.5194/se-12-1987-2021, 2021
Short summary
Short summary
A new analogue modelling approach was used to simulate the influence of tectonic extension and tilting of the basin floor on salt tectonics in rift basins. Our results show that downward salt flow and gravity gliding takes place if the flanks of the rift basin are tilted. Thus, extension occurs at the basin margins, which is compensated for by reduced extension and later by shortening in the graben centre. These outcomes improve the reconstruction of salt-related structures in rift basins.
This article is included in the Encyclopedia of Geosciences
Torsten Hundebøl Hansen, Ole Rønø Clausen, and Katrine Juul Andresen
Solid Earth, 12, 1719–1747, https://doi.org/10.5194/se-12-1719-2021, https://doi.org/10.5194/se-12-1719-2021, 2021
Short summary
Short summary
We have analysed the role of deep salt layers during tectonic shortening of a group of sedimentary basins buried below the North Sea. Due to the ability of salt to flow over geological timescales, the salt layers are much weaker than the surrounding rocks during tectonic deformation. Therefore, complex structures formed mainly where salt was present in our study area. Our results align with findings from other basins and experiments, underlining the importance of salt tectonics.
This article is included in the Encyclopedia of Geosciences
Frank Zwaan, Pauline Chenin, Duncan Erratt, Gianreto Manatschal, and Guido Schreurs
Solid Earth, 12, 1473–1495, https://doi.org/10.5194/se-12-1473-2021, https://doi.org/10.5194/se-12-1473-2021, 2021
Short summary
Short summary
We used laboratory experiments to simulate the early evolution of rift systems, and the influence of structural weaknesses left over from previous tectonic events that can localize new deformation. We find that the orientation and type of such weaknesses can induce complex structures with different orientations during a single phase of rifting, instead of requiring multiple rifting phases. These findings provide a strong incentive to reassess the tectonic history of various natural examples.
This article is included in the Encyclopedia of Geosciences
Laurent Jolivet, Laurent Arbaret, Laetitia Le Pourhiet, Florent Cheval-Garabédian, Vincent Roche, Aurélien Rabillard, and Loïc Labrousse
Solid Earth, 12, 1357–1388, https://doi.org/10.5194/se-12-1357-2021, https://doi.org/10.5194/se-12-1357-2021, 2021
Short summary
Short summary
Although viscosity of the crust largely exceeds that of magmas, we show, based on the Aegean and Tyrrhenian Miocene syn-kinematic plutons, how the intrusion of granites in extensional contexts is controlled by crustal deformation, from magmatic stage to cold mylonites. We show that a simple numerical setup with partial melting in the lower crust in an extensional context leads to the formation of metamorphic core complexes and low-angle detachments reproducing the observed evolution of plutons.
This article is included in the Encyclopedia of Geosciences
Miguel Cisneros, Jaime D. Barnes, Whitney M. Behr, Alissa J. Kotowski, Daniel F. Stockli, and Konstantinos Soukis
Solid Earth, 12, 1335–1355, https://doi.org/10.5194/se-12-1335-2021, https://doi.org/10.5194/se-12-1335-2021, 2021
Short summary
Short summary
Constraining the conditions at which rocks form is crucial for understanding geologic processes. For years, the conditions under which rocks from Syros, Greece, formed have remained enigmatic; yet these rocks are fundamental for understanding processes occurring at the interface between colliding tectonic plates (subduction zones). Here, we constrain conditions under which these rocks formed and show they were transported to the surface adjacent to the down-going (subducting) tectonic plate.
This article is included in the Encyclopedia of Geosciences
Karsten Reiter
Solid Earth, 12, 1287–1307, https://doi.org/10.5194/se-12-1287-2021, https://doi.org/10.5194/se-12-1287-2021, 2021
Short summary
Short summary
The influence and interaction of elastic material properties (Young's modulus, Poisson's ratio), density and low-friction faults on the resulting far-field stress pattern in the Earth's crust is tested with generic models. A Young's modulus contrast can lead to a significant stress rotation. Discontinuities with low friction in homogeneous models change the stress pattern only slightly, away from the fault. In addition, active discontinuities are able to compensate stress rotation.
This article is included in the Encyclopedia of Geosciences
Hilmar von Eynatten, Jonas Kley, István Dunkl, Veit-Enno Hoffmann, and Annemarie Simon
Solid Earth, 12, 935–958, https://doi.org/10.5194/se-12-935-2021, https://doi.org/10.5194/se-12-935-2021, 2021
Eline Le Breton, Sascha Brune, Kamil Ustaszewski, Sabin Zahirovic, Maria Seton, and R. Dietmar Müller
Solid Earth, 12, 885–913, https://doi.org/10.5194/se-12-885-2021, https://doi.org/10.5194/se-12-885-2021, 2021
Short summary
Short summary
The former Piemont–Liguria Ocean, which separated Europe from Africa–Adria in the Jurassic, opened as an arm of the central Atlantic. Using plate reconstructions and geodynamic modeling, we show that the ocean reached only 250 km width between Europe and Adria. Moreover, at least 65 % of the lithosphere subducted into the mantle and/or incorporated into the Alps during convergence in Cretaceous and Cenozoic times comprised highly thinned continental crust, while only 35 % was truly oceanic.
This article is included in the Encyclopedia of Geosciences
Lior Suchoy, Saskia Goes, Benjamin Maunder, Fanny Garel, and Rhodri Davies
Solid Earth, 12, 79–93, https://doi.org/10.5194/se-12-79-2021, https://doi.org/10.5194/se-12-79-2021, 2021
Short summary
Short summary
We use 2D numerical models to highlight the role of basal drag in subduction force balance. We show that basal drag can significantly affect velocities and evolution in our simulations and suggest an explanation as to why there are no trends in plate velocities with age in the Cenozoic subduction record (which we extracted from recent reconstruction using GPlates). The insights into the role of basal drag will help set up global models of plate dynamics or specific regional subduction models.
This article is included in the Encyclopedia of Geosciences
William Bosworth and Gábor Tari
Solid Earth, 12, 59–77, https://doi.org/10.5194/se-12-59-2021, https://doi.org/10.5194/se-12-59-2021, 2021
Short summary
Short summary
Many of the world's hydrocarbon resources are found in rifted sedimentary basins. Some rifts experience multiple phases of extension and inversion. This results in complicated oil and gas generation, migration, and entrapment histories. We present examples of basins in the Western Desert of Egypt and the western Black Sea that were inverted multiple times, sometimes separated by additional phases of extension. We then discuss how these complex deformation histories impact exploration campaigns.
This article is included in the Encyclopedia of Geosciences
Samuel Mock, Christoph von Hagke, Fritz Schlunegger, István Dunkl, and Marco Herwegh
Solid Earth, 11, 1823–1847, https://doi.org/10.5194/se-11-1823-2020, https://doi.org/10.5194/se-11-1823-2020, 2020
Short summary
Short summary
Based on thermochronological data, we infer thrusting along-strike the northern rim of the Central Alps between 12–4 Ma. While the lithology influences the pattern of thrusting at the local scale, we observe that thrusting in the foreland is a long-wavelength feature occurring between Lake Geneva and Salzburg. This coincides with the geometry and dynamics of the attached lithospheric slab at depth. Thus, thrusting in the foreland is at least partly linked to changes in slab dynamics.
This article is included in the Encyclopedia of Geosciences
Paul Angrand, Frédéric Mouthereau, Emmanuel Masini, and Riccardo Asti
Solid Earth, 11, 1313–1332, https://doi.org/10.5194/se-11-1313-2020, https://doi.org/10.5194/se-11-1313-2020, 2020
Short summary
Short summary
We study the Iberian plate motion, from the late Permian to middle Cretaceous. During this time interval, two oceanic systems opened. Geological evidence shows that the Iberian domain preserved the propagation of these two rift systems well. We use geological evidence and pre-existing kinematic models to propose a coherent kinematic model of Iberia that considers both the Neotethyan and Atlantic evolutions. Our model shows that the Europe–Iberia plate boundary was made of two rift systems.
This article is included in the Encyclopedia of Geosciences
Daniel Pastor-Galán, Gabriel Gutiérrez-Alonso, and Arlo B. Weil
Solid Earth, 11, 1247–1273, https://doi.org/10.5194/se-11-1247-2020, https://doi.org/10.5194/se-11-1247-2020, 2020
Short summary
Short summary
Pangea was assembled during Devonian to early Permian times and resulted in a large-scale and winding orogeny that today transects Europe, northwestern Africa, and eastern North America. This orogen is characterized by an
This article is included in the Encyclopedia of Geosciences
Sshape corrugated geometry in Iberia. This paper presents the advances and milestones in our understanding of the geometry and kinematics of the Central Iberian curve from the last decade with particular attention paid to structural and paleomagnetic studies.
Richard Spitz, Arthur Bauville, Jean-Luc Epard, Boris J. P. Kaus, Anton A. Popov, and Stefan M. Schmalholz
Solid Earth, 11, 999–1026, https://doi.org/10.5194/se-11-999-2020, https://doi.org/10.5194/se-11-999-2020, 2020
Short summary
Short summary
We apply three-dimensional (3D) thermo-mechanical numerical simulations of the shortening of the upper crustal region of a passive margin in order to investigate the control of 3D laterally variable inherited structures on fold-and-thrust belt evolution and associated nappe formation. The model is applied to the Helvetic nappe system of the Swiss Alps. Our results show a 3D reconstruction of the first-order tectonic evolution showing the fundamental importance of inherited geological structures.
This article is included in the Encyclopedia of Geosciences
Manfred Lafosse, Elia d'Acremont, Alain Rabaute, Ferran Estrada, Martin Jollivet-Castelot, Juan Tomas Vazquez, Jesus Galindo-Zaldivar, Gemma Ercilla, Belen Alonso, Jeroen Smit, Abdellah Ammar, and Christian Gorini
Solid Earth, 11, 741–765, https://doi.org/10.5194/se-11-741-2020, https://doi.org/10.5194/se-11-741-2020, 2020
Short summary
Short summary
The Alboran Sea is one of the most active region of the Mediterranean Sea. There, the basin architecture records the effect of the Africa–Eurasia plates convergence. We evidence a Pliocene transpression and a more recent Pleistocene tectonic reorganization. We propose that main driving force of the deformation is the Africa–Eurasia convergence, rather than other geodynamical processes. It highlights the evolution and the geometry of the present-day Africa–Eurasia plate boundary.
This article is included in the Encyclopedia of Geosciences
Dan J. Clark, Sarah Brennand, Gregory Brenn, Matthew C. Garthwaite, Jesse Dimech, Trevor I. Allen, and Sean Standen
Solid Earth, 11, 691–717, https://doi.org/10.5194/se-11-691-2020, https://doi.org/10.5194/se-11-691-2020, 2020
Short summary
Short summary
A magnitude 5.3 reverse-faulting earthquake in September 2018 near Lake Muir in southwest Western Australia was followed after 2 months by a collocated magnitude 5.2 strike-slip event. The first event produced a ~ 5 km long and up to 0.5 m high west-facing surface rupture, and the second triggered event deformed but did not rupture the surface. The earthquake sequence was the ninth to have produced surface rupture in Australia. None of these show evidence for prior Quaternary surface rupture.
This article is included in the Encyclopedia of Geosciences
Craig Magee and Christopher Aiden-Lee Jackson
Solid Earth, 11, 579–606, https://doi.org/10.5194/se-11-579-2020, https://doi.org/10.5194/se-11-579-2020, 2020
Short summary
Short summary
Injection of vertical sheets of magma (dyke swarms) controls tectonic and volcanic processes on Earth and other planets. Yet we know little of the 3D structure of dyke swarms. We use seismic reflection data, which provides ultrasound-like images of Earth's subsurface, to study a dyke swarm in 3D for the first time. We show that (1) dyke injection occurred in the Late Jurassic, (2) our data support previous models of dyke shape, and (3) seismic data provides a new way to view and study dykes.
This article is included in the Encyclopedia of Geosciences
Emmanuelle Ricchi, Christian A. Bergemann, Edwin Gnos, Alfons Berger, Daniela Rubatto, Martin J. Whitehouse, and Franz Walter
Solid Earth, 11, 437–467, https://doi.org/10.5194/se-11-437-2020, https://doi.org/10.5194/se-11-437-2020, 2020
Short summary
Short summary
This study investigates Cenozoic deformation during cooling and exhumation of the Tauern metamorphic and structural dome, Eastern Alps, through Th–Pb dating of fissure monazite-(Ce). Fissure (or hydrothermal) monazite-(Ce) typically crystallizes in a temperature range of 400–200 °C. Three major episodes of monazite growth occurred at approximately 21, 17, and 12 Ma, corroborating previous crystallization and cooling ages.
This article is included in the Encyclopedia of Geosciences
Annabel Causer, Lucía Pérez-Díaz, Jürgen Adam, and Graeme Eagles
Solid Earth, 11, 397–417, https://doi.org/10.5194/se-11-397-2020, https://doi.org/10.5194/se-11-397-2020, 2020
Short summary
Short summary
Here we discuss the validity of so-called “break-up” markers along the Newfoundland margin, challenging their perceived suitability for plate kinematic reconstructions of the southern North Atlantic. We do this on the basis of newly available seismic transects across the Southern Newfoundland Basin. Our new data contradicts current interpretations of the extent of oceanic lithosphere and illustrates the need for a differently constraining the plate kinematics of the Iberian plate pre M0 times.
This article is included in the Encyclopedia of Geosciences
Dániel Kiss, Thibault Duretz, and Stefan Markus Schmalholz
Solid Earth, 11, 287–305, https://doi.org/10.5194/se-11-287-2020, https://doi.org/10.5194/se-11-287-2020, 2020
Short summary
Short summary
In this paper, we investigate the physical mechanisms of tectonic nappe formation by high-resolution numerical modeling. Tectonic nappes are key structural features of many mountain chains which are packets of rocks displaced, sometimes even up to 100 km, from their original position. However, the physical mechanisms involved are not fully understood. We solve numerical equations of fluid and solid dynamics to improve our knowledge. The results are compared with data from the Helvetic Alps.
This article is included in the Encyclopedia of Geosciences
Diane Arcay, Serge Lallemand, Sarah Abecassis, and Fanny Garel
Solid Earth, 11, 37–62, https://doi.org/10.5194/se-11-37-2020, https://doi.org/10.5194/se-11-37-2020, 2020
Short summary
Short summary
We propose a new exploration of the concept of
This article is included in the Encyclopedia of Geosciences
spontaneouslithospheric collapse at a transform fault (TF) by performing a large study of conditions allowing instability of the thicker plate using 2-D thermomechanical simulations. Spontaneous subduction is modelled only if extreme mechanical conditions are assumed. We conclude that spontaneous collapse of the thick older plate at a TF evolving into mature subduction is an unlikely process of subduction initiation at modern Earth conditions.
Menno Fraters, Cedric Thieulot, Arie van den Berg, and Wim Spakman
Solid Earth, 10, 1785–1807, https://doi.org/10.5194/se-10-1785-2019, https://doi.org/10.5194/se-10-1785-2019, 2019
Short summary
Short summary
Three-dimensional numerical modelling of geodynamic processes may benefit strongly from using realistic 3-D starting models that approximate, e.g. natural subduction settings in the geological past or at present. To this end, we developed the Geodynamic World Builder (GWB), which enables relatively straightforward parameterization of complex 3-D geometric structures associated with geodynamic processes. The GWB is an open-source community code designed to easily interface with geodynamic codes.
This article is included in the Encyclopedia of Geosciences
Fabio Trippetta, Patrizio Petricca, Andrea Billi, Cristiano Collettini, Marco Cuffaro, Anna Maria Lombardi, Davide Scrocca, Giancarlo Ventura, Andrea Morgante, and Carlo Doglioni
Solid Earth, 10, 1555–1579, https://doi.org/10.5194/se-10-1555-2019, https://doi.org/10.5194/se-10-1555-2019, 2019
Short summary
Short summary
Considering all mapped faults in Italy, empirical scaling laws between fault dimensions and earthquake magnitude are used at the national scale. Results are compared with earthquake catalogues. The consistency between our results and the catalogues gives credibility to the method. Some large differences between the two datasets suggest the validation of this experiment elsewhere.
This article is included in the Encyclopedia of Geosciences
Károly Hidas, Carlos J. Garrido, Guillermo Booth-Rea, Claudio Marchesi, Jean-Louis Bodinier, Jean-Marie Dautria, Amina Louni-Hacini, and Abla Azzouni-Sekkal
Solid Earth, 10, 1099–1121, https://doi.org/10.5194/se-10-1099-2019, https://doi.org/10.5194/se-10-1099-2019, 2019
Short summary
Short summary
Subduction-transform edge propagator (STEP) faults are the locus of continual lithospheric tearing at the edges of subducted slabs, resulting in sharp changes in the lithospheric thickness and triggering lateral and/or near-vertical mantle flow. Here, we study upper mantle rocks recovered from a STEP fault context by < 4 Ma alkali volcanism. We reconstruct how the microstructure developed during deformation and coupled melt–rock interaction, which are promoted by lithospheric tearing at depth.
This article is included in the Encyclopedia of Geosciences
Frank Zwaan, Guido Schreurs, and Susanne J. H. Buiter
Solid Earth, 10, 1063–1097, https://doi.org/10.5194/se-10-1063-2019, https://doi.org/10.5194/se-10-1063-2019, 2019
Short summary
Short summary
This work was inspired by an effort to numerically reproduce laboratory models of extension tectonics. We tested various set-ups to find a suitable analogue model and in the process systematically charted the impact of set-ups and boundary conditions on model results, a topic poorly described in existing scientific literature. We hope that our model results and the discussion on which specific tectonic settings they could represent may serve as a guide for future (analogue) modeling studies.
This article is included in the Encyclopedia of Geosciences
Cited articles
Abdelmalak, M. M., Dubois, C., Mourgues, R., Galland, O., Legland, J.-B.,
and Gruber, C.: Description of new dry granular materials of variable
cohesion and friction coefficient: Implications for laboratory modeling of
the brittle crust, Tectonophysics 684, 39–51,
https://doi.org/10.1016/j.tecto.2016.03.003, 2016.
Adam, J., Urai, J. L., Wieneke, B., Oncken, O., Pfeiffer, K., Kukowski, N.,
and Lohrmann, J.: Shear localisation and strain distribution during tectonic
faulting – new insights from granular-flow experiments and high-resolution
optical image correlation techniques, J. Struct. Geol., 27, 283–301,
https://doi.org/10.1016/j.jsg.2004.08.008, 2005.
Adam, J., Klinkmüller, M., Schreurs, G., and Wieneke, B.: Quantitative
3D strain analysis in analogue experiments simulating tectonic deformation:
Integration of X-ray computed tomography and digital volume correlation
techniques, J. Struct. Geol., 55, 127–149,
https://doi.org/10.1016/j.jsg.2013.07.011, 2013.
Agostini, A., Corti, G., Zeoli, A., and Mulugeta, G.: Evolution, pattern,
and partitioning of deformation during oblique continental rifting:
Inferences from lithospheric-scale centrifuge models, Geochem. Geophy.
Geosy., 10, Q11015, https://doi.org/10.1029/2009GC002676, 2009.
Allemand, P. and Brun, J.-P.: Width of continental rifts and rheological
layering of the lithosphere, Tectonophysics, 188, 63–69,
https://doi.org/10.1016/0040-1951(91)90314-I, 1991.
Allemand, P., Brun, J.-P., Davy P., and Van den Driessche, J.: Symétrie
et asymétrie des rifts et mécanismes d'amincissement de la
lithospère, Bull. Soc. géol. France, 8, 445–451,
https://doi.org/10.2113/gssgfbull.V.3.445, 1989.
Almqvist, B. S. G. and Koyi, H.: Bulk strain in orogenic wedges based on
insights from magnetic fabrics in sandbox models, Geology, 46, 483–486,
https://doi.org/10.1130/G39998.1, 2018.
Amilibia, A., McClay, K. R., Sàbat, F, Muñoz, J. A., and Roca, E.:
Analogue modelling of inverted oblique rift systems, Geol. Acta, 3, 251–271,
https://revistes.ub.edu/index.php/GEOACTA/article/view/105.000001395/4178 (last access: 22 October 2022), 2005.
Angrand, P., Mouthereau, F., Masini, E., and Asti, R.: A reconstruction of
Iberia accounting for Western Tethys–North Atlantic kinematics since the
late-Permian–Triassic, Solid Earth, 11, 1313–1332,
https://doi.org/10.5194/se-11-1313-2020, 2020.
ArRajehi, A., McClusky, S., Reilinger, R., Daoud, M., Alchalbi, A.,
Ergintav, S., Gomez, F., Sholan, J., Bou-Rabee, F., Ogubazghi, G., Haileab,
B., Fisseha, S., Asfaw, L., Mahmoud, S., Rayan, A., Bendik, R., and Kogan,
L.: Geodetic constraints on present-day motion of the Arabian Plate:
Implications for Red Sea and Gulf of Aden rifting, Tectonics, 29, TC3011,
https://doi.org/10.1029/2009TC002482, 2010.
Arch, J., Maltman, A. J., and Knipe, R. J.: Shear zone geometries in
experimentally deformed clays: the influence of water content, strain rate
and primary fabric, J. Struct. Geol., 10, 91–99,
https://doi.org/10.1016/0191-8141(88)90131-9, 1988.
Arthur, J. R. F., Dunstan, T., Al-Ani, Q. A. J., and Assadi, A.: Plastic
deformation and failure of granular media, Geìotechnique, 27, 53–74,
https://doi.org/10.1680/geot.1977.27.1.53, 1977.
Badley, M. E., Price, J. D., and Backshall, L. C.: Inversion, reactivated
faults and related structures: seismic examples from the southern North Sea,
Geol. Soc. Spec. Publ., 44, 201–219,
https://doi.org/10.1144/GSL.SP.1989.044.01.12, 1989.
Bahroudi, A., Koyi, H., and Talbot, C. J.: Effect of ductile and frictional
décollements on style of extension, J. Struct. Geol., 25, 1401–1423,
https://doi.org/10.1016/S0191-8141(02)00201-8, 2003.
Barrientos, B., Cerca, M., Carcía-Márquez, J., and
Hernández-Bernal, C.: Three-dimensional displacement fields measured in
a deforming granular-media surface by combined fringe projection and speckle
photography, J. Opt. A-Pure. Appl. Opt., 10, 104027,
https://doi.org/10.1088/1464-4258/10/10/104027, 2008.
Békési, E., Struijk, M., Bonté, D., Veldkamp, H., Limberger, J.,
Fokker, P. A., Vrijlandt, M., and Van Wees, J.-D.: An updated geothermal
model of the Dutch subsurface based on inversion of temperature data,
Geothermics, 88, 101880,
https://doi.org/10.1016/j.geothermics.2020.101880, 2020.
Bellahsen, N. and Daniel, J.-M.: Fault reactivation control on normal fault
growth: An experimental study, J. Struct. Geol., 27, 769–780,
https://doi.prg/10.1016/j.jsg.2004.12.003, 2005.
Bellahsen, N., Daniel, J., Bollinger, L., and Burov, E. B. E.: Influence of
viscous layers on the growth of normal faults: insights from experimental
and numerical models, J. Struct. Geol., 25, 1471–1485,
https://doi.org/10.1016/s0191-8141(02)00185-2, 2003.
Benes, V. and Scott, S. D.: Oblique rifting in the Havre Trough and its
propagation into the continental margin of New Zealand: Comparison with
analogue experiments, Mar. Geophys. Res., 18, 189–201,
https://doi.org/10.1007/BF00286077, 1996.
Beniest, A., Willingshofer, E., Sokoutis, D., and Sassi, W.: Extending
continental lithosphere with lateral strength variations: effects on
deformation localization and margin geometries, Front. Earth Sci., 6, 148,
https://doi.org/10.3389/feart.2018.00148, 2018.
Bonini, M.: Chronology of deformation and analogue modelling of the
Plio-Pleistocene “Tiber Basin” implications for the evolution of the
Northern Apennines (Italy), Tectonophysics, 285, 147–165,
https://doi.org/10.1016/S0040-1951(97)00189-3, 1998.
Bonini, M., Souriot, T., Boccaletti, M., and Brun, J.-P.: Successive
orthogonal and oblique extension episodes in a rift zone: Laboratory
experiments with application to the Ethiopian Rift, Tectonics, 16, 347–362,
https://doi.org/10.1029/96TC03935, 1997.
Bonini, M., Sani, F., and Antonielli, B.: Basin inversion and contractional
reactivation of inherited normal faults: A review based on previous and new
experimental models, Tectonophysics, 522/523, 55–88,
https://doi.org/10.1016/j.tecto.2011.11.014, 2012.
Borderie, S., Graveleau, F., Witt, C., and Vendeville, B. C.: Impact of an
interbedded viscous décollement on the structural and kinematic coupling
in fold-and-thrust belts: Insights from analogue modeling, Tectonophysics,
722, 118–137, https://doi.org/10.1016/j.tecto.2017.10.019, 2018.
Borderie, S., Vendeville, B. C., Graveleau, F., Witt, C., Dubois, P., Baby,
P., and Calderon, Y.: Analogue modeling of large-transport thrust faults in
evaporites-floored basins: Example of the Chazuta Thrust in the Huallaga
Basin, Peru, J. Struct. Geol., 123, 1–17,
https://doi.org/10.1016/j.jsg.2019.03.002, 2019.
Bosworth, W. and Tari, G.: Hydrocarbon accumulation in basins with multiple
phases of extension and inversion: Examples from the Western Desert (Egypt)
and the western Black Sea, Solid Earth, 12, 59–77,
https://doi.org/10.5194/se-12-59-2021, 2021.
Boutelier, D. and Oncken, O.: 3-D thermo-mechanical laboratory modeling of
plate-tectonics: Modeling scheme, technique and first experiments, Solid
Earth, 2, 35–51, https://doi.org/10.5194/se-2-35-2011, 2011.
Boutelier, D., Oncken, O., and Cruden, S.: Fore-arc deformation at the
transition between collision and subduction: Insights from 3-D
thermomechanical laboratory experiments, Tectonics, 31, TC2015,
https://doi.org/10.1029/2011TC003060, 2012.
Boutelier, D., Schrank, C., and Regenauer-Lieb, K.: 2-D finite displacements
and finite strain from PIV analysis of plane-strain tectonic analogue
models, Solid Earth, 10, 1123–1139,
https://doi.org/10.5194/se-10-1123-2019, 2019.
Boutoux, A., Biraud, A., Facenna, C., Ballato, P., Rossetti, F., and Blanc,
F.: Slab folding and surface deformation of the Iran mobile belt, Tectonics,
40, e2020TC006300, https://doi.org/10.1029/2020TC006300, 2021.
Broerse, T., Krstekanić, N., Kasbergen, C., and Willingshofer, E.:
Mapping and classifying large deformation from digital imagery: application
to analogue models of lithosphere deformation, Geophys. J. Int., 226,
984–1017, https://doi.org/10.1093/gji/ggab120, 2021.
Brun, J.-P.: Narrow rifts versus wide rifts: inferences for the mechanics of
rifting from laboratory experiments, Philos. T. R. Soc. Lond. A, 357,
695–712, https://doi.org/10.1098/rsta.1999.0349, 1999.
Brun, J.-P.: Deformation of the continental lithosphere: Insights from
brittle-ductile models, Geol. Soc. Spec. Publ., 200, 355–370,
https://doi.org/10.1144/GSL.SP.2001.200.01.20, 2002.
Brun, J.-P. and Beslier, M. O.: Mantle exhumation at passive margins, Earth
Planet. Sci. Lett., 142, 161–173.
https://doi.org/10.1016/0012-821x(96)00080-5, 1996.
Brun, J.-P. and Nalpas, T.: Graben inversion in nature and experiments,
Tectonics, 15, 677–687, https://doi.org/10.1029/95TC03853, 1996.
Brun, J.-P. and Tron, V.: Development of the North Viking Graben: inferences
from laboratory modelling, Sediment. Geol., 86, 31–51,
https://doi.org/10.1016/0037-0738(93)90132-O, 1993.
Brune, S., Williams, S. E., Butterworth, N. P., and Müller, R. D.:
Abrupt plate accelerations shape rifted continental margins, Nature, 536,
201–204, https://doi.org/10.1038/nature18319, 2016.
Brune, S., Corti, G., and Ranalli, G.: Controls of inherited lithospheric
heterogeneity on rift linkage: Numerical and analogue models of interaction
between the Kenyan and Ethiopian rifts across the Turkana depression,
Tectonics, 36, 1767–1786,
https://doi.org/10.1002/2017TC004739, 2017.
Brune, S., Williams, S. E., and Müller, R. D.: Oblique rifting: the
rule, not the exception, Solid Earth, 9, 1187–1206,
https://doi.org/10.5194/se-9-1187-2018, 2018.
Buchanan, P. G. and McClay, K. R.: Sandbox experiments of inverted listric
and planar fault systems, Tectonophysics, 188, 97–115,
https://doi.org/10.1016/0040-1951(91)90317-L, 1991.
Buchanan, J. G. and Buchanan, P. G. (Eds.): Basin Inversion, Geol. Soc. Spec.
Publ., 88, Geological Society, London, UK, 596 pp.,
https://doi.org/10.1144/GSL.SP.1995.088.01.30, 1995.
Buchanan, P. G. and McClay, K. R.: Experiments on basin inversion above
reactivated domino faults, Mar. Pet. Geol., 9, 486–500,
https://doi.org/10.1016/0264-8172(92)90061-I, 1992.
Buck, W. R.: Modes of continental lithospheric extension, J. Geophys. Res.,
96, 20161, https://doi.org/10.1029/91JB01485, 1991.
Buiter, S. J. H.: A review of brittle compressional wedge models,
Tectonophysics, 530/531, 1–17,
https://doi.org/10.1016/j.tecto.2011.12.018, 2012.
Buiter, S. J. H. and Pfiffner, O. A.: Numerical models of the inversion of
half-graben basins, Tectonics, 22, 1057,
https://doi.org/10.1029/2002TC001417, 2003.
Buiter, S. J. H., Babeyko, A. Y., Ellis, S., Gerya, T. V., Kaus, B. J. P.,
Kellner, A., Schreurs, G., and Yamada, Y.: The numerical sandbox: Comparison
of model results for a shortening and an extension experiment, Geol. Soc.
Spec. Publ., 253, 29–64,
https://doi.org/10.1144/GSL.SP.2006.253.01.02, 2006.
Buiter, S. J. H., Huismans, R. S., and Beaumont, C.: Dissipation analysis as
a guide to mode selection during crustal extension and implications for the
styles of sedimentary basins, J. Geophys. Res., 113, B06406,
https://doi.org/10.1029/2007JB005272, 2008.
Buiter, S. J. H., Pfiffner, O. A., and Beaumont, C.: Inversion of
extensional sedimentary basins: A numerical evaluation of the localisation
of shortening, Earth Planet. Sc. Lett., 288, 492–504,
https://doi.org/10.1016/j.epsl.2009.10.011, 2009.
Buiter, S. J. H., Schreurs, G., Albertz, M., Gerya, T. V., Kaus, B., Landry,
W., le Pourhiet, L., Mishin, Y., Egholm, D. L., Cooke, M., Maillot, B.,
Thiuelot, C., Crook, T., May, D., Souloumiac, P., and Beaumont, C.:
Benchmarking numerical models of brittle thrust wedges, J. Struct. Geol.,
92, 140–177, https://doi.org/10.1016/j.jsg.2016.03.003, 2016.
Burliga, S., Koyi, H. A., and Chemia, Z.: Analogue and numerical modelling
of salt supply to a diapiric structure rising above an active basement
fault, Geol. Soc. Spec. Publ., 363, 395–408,
https://doi.org/10.1144/SP363.18, 2012a.
Burliga, S., Koyi, H. A., and Krzywiec, P.: Modelling cover deformation and
decoupling during inversion, using the Mid-Polish Trough as a case study, J.
Struct. Geol., 42, 62–73,
https://doi.org/10.1016/j.jsg.2012.06.013, 2012b.
Burov, E. B. E. and Cloetingh, S.: Post-Rift Evolution of Extensional
Basins, Earth Planet. Sc. Lett., 150, 7–26,
https://doi.org/10.1016/S0012-821X(97)00069-1, 1997.
Byerlee, J.: Friction of Rocks, Pure Appl. Geophys., 116, 615–626,
https://doi.org/10.1007/BF00876528, 1978.
Cadell, H. M.: Experimental researches in mountain building, T.
R. Soc. Edinburgh, 35, 337–357,
https://doi.org/10.1017/S0080456800017658, 1889.
Caër, T., Maillot, B., Souloumiac, P., Leturmy, P., Frizon de Lamotte,
D., and Nussbaum, C.: Mechanical validation of balanced cross-sections: The
case of the Mont Terri anticline at the Jura front (NW Switzerland), J.
Struct. Geol., 75, 32–48,
https://doi.org/10.1016/j.jsg.2015.03.009, 2015.
Calignano, E., Sokoutis, D., Willingshofer, E., Gueydan, F., and Cloetingh,
S.: Asymmetric vs. symmetric deep lithospheric architecture of intra-plate
continental orogens, Earth Planet. Sc. Lett., 424, 38–50,
https://doi.org/10.1016/j.epsl.2015.05.022, 2015.
Calignano, E., Sokoutis, D., Willingshofer, E., Brun, J.-P., Gueydan, F.,
and Cloetingh, S.: Oblique contractional reactivation of inherited
heterogeneities: Cause for arcuate orogens, Tectonics, 36, 542–558,
https://doi.org/10.1002/2016TC004424, 2017.
Cerca, M., Ferrari, L., Corti, G., Bonini, M., and Manetti, P.: Analogue
model of inversion tectonics explaining the structural diversity of Late
Cretaceous shortening in southwestern Mexico, Lithosphere, 2, 172–187,
https://doi.org/10.1130/L48.1, 2010.
Chauvin, B. P., Lovely, P. J., Stockmeyer, J. M., Plesch, A., Caumon, G.,
and Shaw, J. H.: Validating novel boundary conditions for three-dimensional
mechanics-based restoration: An extensional sandbox model example, AAPG
Bull., 102, 245–256, https://doi.org/10.1306/0504171620817154, 2018.
Chemenda, A., DeìvercheÌre, J., and Calais, E.: Three-dimensional
laboratory modelling of rifting: Application to the Baikal Rift, Russia,
Tectonophysics, 356, 253–273,
https://doi.org/10.1016/S0040-1951(02)00389-X, 2002.
Cobbold, P. R., Durand, S., and Mourgues, R.: Sandbox modelling of thrust wedges
with fluid-assisted detachments, Tectonophysics, 334, 245–258,
https://doi.org/10.1016/S0040-1951(01)00070-1, 2001.
Colletta, B., Letouzey, J., Pinedo, R., Ballard, J. F., and Bale, P.:
Computerized X-ray tomography analysis of sandbox models: examples of
thin-skinned thrust systems, Geology, 19, 1063–1067,
https://doi.org/10.1130/0091-7613(1991)019<1063:CXRTAO>2.3.CO;2, 1991.
Cooper, M. A. and Williams, G. D. (Eds.): Inversion tectonics, Geol. Soc.
Spec. Publ., 44, Geological Society, London, UK, 375 pp.,
https://doi.org/10.1144/GSL.SP.1989.044.01.25, 1989.
Cooper, M. and Warren, M. J.: The geometric characteristics, genesis and
petroleum significance of inversion structures, Geol. Soc. Spec. Publ., 335,
827–846, https://doi.org/10.1144/SP335.33, 2010.
Cooper, M. and Warren, M. J.: Inverted fault systems and inversion tectonic
settings, in: Regional Geology and Tectonics, edited by: Scarselli, N.,
Adam, J., Chiarella, D., Roberts, D. G., and Bally, A. W., Elsevier,
169–204, https://doi.org/10.1016/B978-0-444-64134-2.00009-2, 2020.
Cooper, M. A., Williams, G. D., De Graciansky, P. C., Murphy, R. W.,
Needham, T., De Paor, D., Stoneley, R., Todd, S. P., Turner, J. P., and
Ziegler, P. A.: Inversion tectonics – a discussion, Geol. Soc. Spec. Publ.,
44, 335–347, https://doi.org/10.1144/GSL.SP.1989.044.01.18, 1989.
Corbi, F., Sandri, L., Bedford, J., Funiciello, F., Brizzi, S., Rosenau, M.,
and Lallemand, S.: Machine learning can predict the timing and size of
analog earthquakes, Geophys. Res. Lett., 46, 1303–1311,
https://doi.org/10.1029/2018GL081251, 2019.
Corti, G.: Evolution and characteristics of continental rifting: Analog modeling-inspired view and
comparison with examples from the East African Rift System, Tectonophysics, 522/523, 1–33,
https://doi.org/10.1016/j.tecto.2011.06.010, 2012.
Corti, G., Bonini, M., Conticelli, S., Innocenti, F., Manetti, P., and
Sokoutis, D.: Analogue modelling of continental extension: A review focused
on the relations between the patterns of deformation and the presence of
magma, Earth-Sci. Rev., 63, 169–247,
https://doi.org/10.1016/S0012-8252(03)00035-7, 2003.
Corti, G., Bonini, M., Sokoutis, D., Innocenti, F., Manetti, P., Cloetingh,
S., and Mulugeta, G.: Continental rift architecture and patterns of magma
migration: A dynamic analysis based on centrifuge models, Tectonics, 23,
TC2012, https://doi.org/10.1029/2003TC001561, 2004.
Corti, G., van Wijk, J. W., Cloetingh, S., and Morley, C. K.: Tectonic
inheritance and continental rift architecture: Numerical and analogue models
of the East African Rift system, Tectonics, 26, 1–13,
https://doi.org/10.1029/2006TC002086, 2007.
Cotton, J. T. and Koyi, H. A.: Modeling of thrust fronts above ductile and
frictional detachments: Application to structures in the Salt Range and
Potwar Plateau, Pakistan, GSA Bull., 112, 351–363,
https://doi.org/10.1130/0016-7606(2000)112<351:MOTFAD>2.0.CO;2, 2000.
Coulomb, C. A.: L'application des règles de maximis et minimis à
quelques problèmes de statique, relatifs à l'architecture,
Mémoires de Mathématique et de Physique, Academie Royale des
Sciences, 7, 343–382, 1773.
Crook, A. J. L, Willson, S. M., Yu, J. G., and Owen, D. R. J: Predictive
modelling of structure evolution in sandbox experiments, J. Struct. Geol.,
28, 729–744, https://doi.org/10.1016/j.jsg.2006.02.002, 2006.
Cruz, L., Malinski, A., Tae, W. A., and Hilley, G.: Erosional control of the
kinematics and geometry of fold-and-thrust belts imaged in a physical and
numerical sandbox, J. Geophys. Res., 115, B09404,
https://doi.org/10.1029/2010JB007472, 2010.
Dai, L., Li, S., Lou, D., Liu, X., Suo, Y., and Yu, S.: Numerical modeling
of Late Miocene tectonic inversion in the Xihu Sag, East China Sea Shelf
Basin, China, J. Asian Earth Sci., 86, 25–37,
https://doi.org/10.1016/j.jseaes.2013.09.033, 2014.
Daniels, K. E., Kollmer, J. E., and Puckett, J. G.: Photoelastic force
measurements in granular materials, Rev. Sci. Instrum., 88, 051808,
https://doi.org/10.1063/1.4983049, 2017.
Deckers, J., Rombaut, B., Van Noten, K., and Vanneste, K.: Influence of
inherited structural domains and their particular strain distributions on
the Roer Valley graben evolution?from inversion to extension, Solid Earth,
12, 345–361, https://doi.org/10.5194/se-12-345-2021, 2021.
De Jager, J.: Inverted basins in the Netherlands, similarities and
differences, Neth. J. Geosci., 82, 355–366,
https://doi.org/10.1017/S0016774600020175, 2003.
De Jager, J. and Geluk, M. C.: Petroleum Geology, in: Geology of the
Netherlands, edited by: Wong, T. E., Batjes, D. A. J., and De Jager, J., Royal
Netherlands Academy of Arts and Sciences, 241–264, ISBN: 9789069844817,
https://www.researchgate.net/publication/312604683 (last access: 22 October 2022), 2007.
Del Ventisette, C., Montanari, D., Bonini, M., and Sani F.: Positive fault
inversion triggering “intrusive diapirism”: an analogue modelling
perspective, Terra Nova, 17, 478–485,
https://doi.org/10.1111/j.1365-3121.2005.00637.x, 2005.
Del Ventisette, C., Montanari, D., Sani, F., and Bonini, M.: Basin inversion
and fault reactivation in laboratory experiments, J. Struct. Geol., 28,
2067–2083, https://doi.org/10.1016/j.jsg.2006.07.012, 2006.
Deng, H., Kyi, H. A., and Zhang, J.: Modelling oblique inversion of
pre-existing grabens, Geol. Soc. Spec. Publ., 487, 263–290,
https://doi.org/10.1144/SP487.5, 2019.
Di Domenica, A., Bonini, L., Calamita, G., Toscani, G., Galuppo, C., and
Seno, S.: Analogue modeling of positive inversion tectonics along
differently oriented pre-thrusting normal faults: An application to the
Central-Northern Apennines of Italy, GSA Bull., 126, 943–955,
https://doi.org/10.1130/B31001.1, 2014.
Di Giuseppe, E., Funiciello, F., Corbi, F., Ranalli, G., and Mojoli, G.:
Gelatins as rock analogs: A systematic study of their rheological and
physical properties, Tectonophysics, 473, 391–403,
https://doi.org/10.1016/j.tecto.2009.03.012, 2009.
Di Giuseppe, E.: Analogue Materials in Experimental Tectonics, Reference
Module in Earth Systems and Environmental Sciences, Elsevier, 1–32,
https://doi.org/10.1016/B978-0-12-409548-9.10909-1, 2018.
Dilek, Y. and Furnes, H.: Ophiolite genesis and global tectonics:
Geochemical and tectonic fingerprinting of ancient oceanic lithosphere, GSA
Bull., 123, 387–411, https://doi.org/10.1130/B30446.1, 2011.
Dooley, T., McClay, K. R., and Pascoe, R.: 3D analogue models of variable
displacement extensional faults: applications to the Revfallet Fault system,
offshore mid-Norway, Geol. Soc. Spec. Publ., 212, 151–167,
https://doi.org/10.1144/GSL.SP.2003.212.01.10, 2003.
Dooley, T. P. and Hudec, M. R.: Extension and inversion of salt-bearing rift
systems, Solid Earth, 11, 1187–1204,
https://doi.org/10.5194/se-11-1187-2020, 2020.
Doornenbal, H. and Stevenson, A. (Eds.): Petroleum Geological Atlas of the
Southern Permian Basin Area, EAGE Publications b.v., Houten,
https://www.nlog.nl/southern-permian-basin-atlas (last access: 22 October 2022), 2010.
Doornenbal, J. C., Kombrink, H., Bouroullec, R., Dalman, R. A. F., De Bruin,
G., Geel, C. R., Houben, A. J. P., Jaarsma, B., Juez-Larré, J.,
Kortekaas, M., Mijnlieff, H. F., Nelskamp, S., Pharaoh, T. C., Ten Veen, J.
H., Ter Borgh, M., Van Ojik, K., Verreussel, R. M. C. H., Verweij, J. M.,
and Vis, G.-J.: New insights on subsurface energy resources in the Southern
North Sea Basin area, Geol. Soc. Spec. Publ., 494, 233–268,
https://doi.org/10.1144/SP494-2018-178, 2019.
Dubois, A., Odonne, F., Massonnat, G., Lebourg, T., and Fabre, R.: Analogue
modelling of fault reactivation: tectonic inversion and oblique
remobilisation of grabens, J. Struct. Geol., 24, 1741–1752,
https://doi.org/10.1016/S0191-8141(01)00129-8, 2002.
Dumagin, E., Truche, L., and Donzeì, F. V.: Natural Hydrogen
Exploration Guide, Geonum Ed.: ISRN GEONUM-NST–2019-01–ENG, 16 pp.,
https://www.researchgate.net/publication/330728855 (last access: 22 October 2022), 2019.
Edwards, B., Kraft, T., Cauzzi, C., Kästli, P., and Wiener, S.: Seismic
monitoring and analysis of deep geothermal projects in St Gallen and Basel,
Switzerland, Geophys. J. Int., 201, 1022–1039,
https://doi.org/10.1093/gji/ggv059, 2015.
Eisenstadt, G. and Sims, D.: Evaluating sand and clay models: do rheological
differences matter?, J. Struct. Geol., 27, 1399–1412,
https://doi.org/10.1016/j.jsg.2005.04.010, 2005.
Eisenstadt, G. and Withjack, M. O.: Estimating inversion: results from clay
models, Geol. Soc. Lond. Spec. Publ., 88, 119–136,
https://doi.org/10.1144/GSL.SP.1995.088.01.08, 1995.
Eisermann, J. O., Göllner, P. L., and Riller, U.: Orogen-scale
transpression accounts for GPS velocities and kinematic partitioning in the
Southern Andes, Commun. Earth Environ., 2, 167,
https://doi.org/10.1038/s43247-021-00241-4, 2021.
Ellis, S., Schreurs, G., and Panien, M.: Comparisons between analogue and
numerical models of thrust wedge development, J. Struct. Geol., 26,
1659–1675, https://doi.org/10.1016/j.jsg.2004.02.012, 2004.
Erratt, D., Thomas, G. M., and Wall, G. R. T.: The evolution of the Central
North Sea Rift, Geol. Soc. Petrol. Conf. Ser., 5, 63–82,
https://doi.org/10.1144/0050063, 1999.
Evans, D., Graham, C., Armour, A., and Bathurst, P. (Eds.): The Millennium
Atlas: Petroleum geology of the central and northern North Sea, Geological
Society of London, UK, https://doi.org/10.1017/S0016756803218124, 2003.
Faul, U. U., Garapicì, G., and Lugovicì, B.: Subcontinental rift
initiation and ocean-continent transitional setting of the Dinarides and
Vardar zone: Evidence from the Krivaja–Konjuh Massif, Bosnia and
Herzegovina, Lithos, 202/203, 283–299,
https://doi.org/10.1016/j.lithos.2014.05.026, 2014.
Fedorik, J., Zwaan, F., Schreurs, G., Toscani, G., Bonini, L., and Seno, S.:
The interaction between strike-slip dominated fault zones and thrust belt
structures: Insights from 4D analogue models, J. Struct. Geol., 122, 89–105,
https://doi.org/10.1016/j.jsg.2019.02.010, 2019.
Ferrer, O., McClay, K., and Sellier, N. C.: Influence of fault geometries
and mechanical anisotropies on the growth and inversion of hanging-wall
synclinal basins: insights from sandbox models and natural examples, Geol.
Soc. Spec. Publ., 439, 487–509, https://doi.org/10.1144/SP439.8, 2016.
Ferrer, O., Carola, E., and McClay, K.: Structural control of inherited salt structures during inversion of a domino basement-fault system from an analogue modelling approach, EGUsphere [preprint], https://doi.org/10.5194/egusphere-2022-1183, 2022a.
Ferrer, O., Santolaria, P., Muñoz, J. A., Granado, P., Roca, E.,
Gratacós, O., and Snidero, M.: Analogue modeling as a tool to assist
seismic structural interpretation in the Andean fold-and-thrust belt, in:
Andean Structural Styles, edited by: Zomora, G. and Mora, A., Elsevier,
43–61, https://doi.org/10.1016/B978-0-323-85175-6.00003-1, 2022b.
Frasca, G., Gueydan, F., Brun, J.-P., and Monieì, P.: Deformation
mechanisms in a continental rift up to mantle exhumation. Field evidence
from the western Betics, Spain, Mar. Petrol. Geol., 76, 310–328,
https://doi.org/10.1016/j.marpetgeo.2016.04.020, 2016.
Gabrielsen, R. H., Sokoutis, D., Willingshofer, E., and Faleide, J. I.:
Fault linkage across weak layers during extension: an experimental approach
with reference to the Hoop Fault Complex of the SW Barents Sea, Petrol.
Geosci., 22, 123–135, https://doi.org/10.1144/petgeo2015-029, 2016.
Gartrell, A., Hudson, C., and Evans, B.: The influence of basement faults
during extension and oblique inversion of the Makassar Straits rift system:
Insights from analog models, AAPG Bull., 89, 495–506,
https://doi.org/10.1306/12010404018, 2005.
Gaucher, E. C.: New Perspectives in the Industrial Exploration for Native
Hydrogen, Elements, 16, 8–9,
https://doi.org/10.2138/gselements.16.1.8, 2020.
Gibson, G. M. and Edwards, S.: Basin inversion and structural architecture
as constraints on fluid flow and Pb–Zn mineralization in the
Paleo–Mesoproterozoic sedimentary sequences of northern Australia, Solid
Earth, 11, 1205–1226, https://doi.org/10.5194/se-11-1205-2020, 2020.
Gibson, G. M., Hutton, L. J., and Holzschuh, J.: Basin inversion and
supercontinent assembly as drivers of sediment-hosted Pb–Zn mineralization
in the Mount Isa region, northern Australia, J. Geol. Soc., 174, 773–786,
https://doi.org/10.1144/jgs2016-105, 2017.
Glennie, K. W. and Boegner, P. L. E.: Sole Pit inversion tectonics, in:
Petroleum Geology of the Continental Shelf of North-West Europe, edited by:
Illing, L. V. and Hobson, G. D., Institute of Petroleum, London, UK,
110–120, ISBN: 9780855016562, 1981.
Gomes, C. J. S., Filho, A. D., Posada, A. M. A., and Da Silva, A. C.: The
role of backstop shape during inversion tectonics physical models, Anais da
Academia Brasileira de Ciéncias, 82, 997–1012,
https://doi.org/10.1590/S0001-37652010000400021, 2010.
Gomes, C. J. S., Martins-Neto, M. A., and Ribeiro, V. A.: Positive inversion
of extensional footwalls in the southern Serra do Espinhaço, Brazil –
insights from sandbox laboratory experiments, Anais da Academia Brasileira
de Ciéncias, 78, 331–334,
https://doi.org/10.1590/S0001-37652006000200012, 2006.
Goudswaard, W. and Jenyon, M. K.: Seismic atlas of structural and
stratigraphic features, European Association of Exploration Geophysicists, 396 pp.,
1988.
Gowers, M. B., Holtar, E., and Swensson, E.: The structure of the Norwegian
Central Trough (Central Graben area), Geol. Soc. Petrol. Conf. Ser., 4,
1245–1254, https://doi.org/10.1144/0041245, 1993.
Granado, P. and Ruh, J. B.: Numerical modelling of inversion tectonics in
fold-and-thrust belts, Tectonophysics, 763, 14–29,
https://doi.org/10.1016/j.tecto.2019.04.033, 2019.
Granado, P., Ferrer, O., Muñoz, J. A., Thöny, W., and Strauss, P.:
Basin inversion in tectonic wedges: Insights from analogue modelling and the
Alpine-Carpathian fold-and-thrust belt, Tectonophysics, 703/704, 50–68,
https://doi.org/10.1016/j.tecto.2017.02.022, 2017.
Graveleau, F. and Dominguez, S.: Analogue modelling of the interaction
between tectonics, erosion and sedimentation in foreland thrust belts, C. R.
Geosci., 340, 324–333,
https://doi.org/10.1016/j.crte.2008.01.005, 2008.
Graveleau, F., Hurtrez, J., Dominguez, S., and Malavieille, J.: A new
experimental material for modeling relief dynamics and interactions between
tectonics and surface processes, Tectonophysics, 513, 68–87,
https://doi.org/10.1016/j.tecto.2011.09.029, 2011.
Graveleau, F., Malavieille, J., and Dominguez, S.: Experimental modelling of
orogenic wedges: A review, Tectonophysics, 538–540, 1–66,
https://doi.org/10.1016/j.tecto.2012.01.027, 2012.
Graveleau, F., Strak, V., Dominguez, S., Malavieille, J., Chatton, M.,
Manighetti, I., and Petit, C.: Experimental modelling of
tectonics-erosion-sedimentation interactions in compressional, extensional,
and strike-slip settings, Geomorphology, 244, 146–168,
https://doi.org/10.1016/j.geomorph.2015.02.011, 2015.
Groves, D. I. and Bierlein, F. P.: Geodynamic settings of mineral deposits,
J. Geol. Soc. London, 164, 19–30,
https://doi.org/10.1144/0016-76492006-065, 2007.
Guillaume, B., Gianni, G. M., Kermarrec, J.-J., and Bock, K.: Control of
crustal strength, tectonic inheritance, and stretching/shortening rates on
crustal deformation and basin reactivation: insights from laboratory models,
Solid Earth, 13, 1393–1414,
https://doi.org/10.5194/se-13-1393-2022, 2022.
Hagemann, S. G., Lisitsin, V. A., and Huston, D. L.: Mineral system
analysis: Quo vadis, Ore Geol. Rev., 76, 504–522,
https://doi.org/10.1016/j.oregeorev.2015.12.012, 2016.
Hall, J. S.: On the vertical position and convolutions of certain strata
and their relation with granite, T. R. Soc.
Edinburgh, 7, 79–108,
https://doi.org/10.1017/S0080456800019268, 1815.
Hansen, D. L. and Nielsen S. B.: Why rifts invert in compression,
Tectonophysics, 373, 5–24,
https://doi.org/10.1016/S0040-1951(03)00280-4, 2003.
Hansen, T. H., Clausen, O. R., and Andersen, K. J.: Thick- and thin-skinned
basin inversion in the Danish Central Graben, North Sea – The role of deep
evaporites and basement kinematics, Solid Earth, 12, 1719–1747,
https://doi.org/10.5194/se-12-1719-2021, 2021.
Herbert, J. W., Cooke, M. L., Souloumiac, P., Madden, E. H., Mary, B. C. L.,
and Maillot, B.: The work of fault growth in laboratory sandbox experiments,
Earth Planet. Sc. Lett., 432, 95–102,
https://doi.org/10.1016/j.epsl.2015.09.046, 2015.
Henza, A. A., Withjack, M. O., and Schlische, R. W.: Normal-fault
development during two phases of non-coaxial extension: An experimental
study, J. Struct. Geol., 32, 1656–1667,
https://doi.org/10.1016/j.jsg.2009.07.007, 2010.
Henza, A. A., Withjack, M. O., and Schlische, R. W.: How do the properties
of a pre-existing normal-fault population influence fault development during
a subsequent phase of extension?, J. Struct. Geol., 33, 1312–1324,
https://doi.org/10.1016/j.jsg.2011.06.010, 2011.
Hubbert, M. K.: Theory of scaled models as applied to the study of
geological structures, Geol. Soc. Am. Bull., 48, 1459–1520,
https://doi.org/10.1130/GSAB-48-1459, 1937.
Hubbert, M. K.: Mechanical basis for certain familiar geologic structures,
GSA Bull., 62, 355–372,
https://doi.org/10.1130/0016-7606(1951)62[355:MBFCFG]2.0.CO;2, 1951.
Hunfeld, L. B., Chen, J., Hol., S., Niemeijer, A. R., and Spiers, C. J.: Healing
Behavior of Simulated Fault Gouges From
the Groningen Gas Field and Implications for Induced Fault Reactivation, J.
Geophys. Res.-Sol. Ea., 123, e2019JB018790,
https://doi.org/10.1029/2019JB018790, 2020.
Iaffa, D. N., Sàbat, F., Bello, D., Ferrer, O., Mon, R., and Gutierrez,
A. A.: Tectonic inversion in a segmented foreland basin from extensional to
piggy back settings: The Tucumán Basin in NW Argentina, J. S. Am. Earth
Sci., 31, 457–474,
https://doi.org/10.1016/j.jsames.2011.02.009, 2011.
Jagger, L. J. and McClay, K.: Analogue modelling of inverted domino-style
basement fault systems, Basin Res., 30, 363–381,
https://doi.org/10.1111/bre.12224, 2016.
Jara, P., Likerman, J., Winocur, D., Ghiglione, M. C., Cristallini, E. O.,
Pinto, L., and Charrier, R.: Role of basin width variation in tectonic
inversion: insight from analogue modelling and implications for the tectonic
inversion of the Abanico Basin, 32∘–34∘ S, Central
Andes, Geol. Soc. Spec. Publ., 399, 83–107,
https://doi.org/10.1144/SP399.7, 2015.
Jara, P., Likerman, J., Charrier R., Herrera, S., Pinto L., Villarroel, M.,
and Winocur, D.: Closure type effects on the structural pattern of an
inverted extensional basin of variable width: Results from analogue models,
J. S. Am. Earth Sci., 87, 157–173,
https://doi.org/10.1016/j.jsames.2017.10.018, 2018.
Katz, R. F., Ragnarsson, R., and Bodenschatz, E.: Tectonic microplates in a
wax model of sea-floor spreading, New J. Phys., 7, 37,
https://doi.org/10.1088/1367-2630/7/1/037, 2005.
Keep, M. and McClay, K.: Analogue modelling of multiphase rift systems,
Tectonophysics, 273, 239–270,
https://doi.org/10.1016/S0040-1951(96)00272-7, 1997.
Keller, J. V. A. and McClay, K. R.: 3D sandbox models of positive inversion,
Geol. Soc. Spec. Publ., 88, 137–146,
https://doi.org/10.1144/GSL.SP.1995.088.01.09, 1995.
Kiss, D., Duretz, T., and Schmalholz, S. M.: Tectonic inheritance controls
nappe detachment, transport and stacking in the Helvetic nappe system,
Switzerland: insights from thermomechanical simulations, Solid Earth, 11,
287–305, https://doi.org/10.5194/se-11-287-2020, 2020.
Klinkmüller, M., Schreurs, G., Rosenau, M., and Kemnitz, H.: Properties
of granular analogue model materials: A community wide survey,
Tectonophysics, 684, 23–38,
https://doi.org/10.1016/j.tecto.2016.01.017, 2016.
Konstantinovskaya, E. A., Harris, L. B., Poulin, J., and Ivanov, G. M.:
Transfer zones and fault reactivation in inverted rift basins: Insights from
physical modelling, Tectonophysics 441, 1–26,
https://doi.org/10.1016/j.tecto.2007.06.002, 2007.
Koons, P. O.: Two-sided orogen: Collision and erosion from the sandbox to
the Southern Alps, New Zealand, Geology, 18, 670–682,
https://doi.org/10.1130/0091-7613(1990)018<0679:TSOCAE>2.3.CO;2, 1990.
Koopman, A., Speksnijder, A., and Horsfield, W. T.: Sandbox model studies of
inversion tectonics, Tectonophysics, 137, 379–388,
https://doi.org/10.1016/0040-1951(87)90329-5, 1987.
Koyi, H. A.: Analogue Modelling: From a Qualitative To a Quantitative
Technique – a Historical Outline, J. Pet. Geol., 20, 223–238,
https://doi.org/10.1111/j.1747-5457.1997.tb00774.x, 1997.
Krantz, R. W.: Normal fault geometry and fault reactivation in tectonic
inversion experiments, Geol. Soc. Spec. Publ., 56, 219–229,
https://doi.org/10.1144/GSL.SP.1991.056.01.15, 1991a.
Krantz, R. W.: Measurements of friction coefficients and cohesion for
faulting and fault reactivation in laboratory models using sand and sand
mixtures, Tectonophysics, 188, 203–207,
https://doi.org/10.1016/0040-1951(91)90323-K, 1991b.
Krstekanicì, N., Willingshofer, E., Broerse, T., Matenco, L.,
Toljicì, and Stojadinovic, U.: Analogue modelling of strain
partitioning along a curved strike-slip fault system during backarc-convex
orocline formation: Implications for the Cerna-Timok fault system of the
Carpatho-Balkanides, J. Struct. Geol., 149, 104386,
https://doi.org/10.1016/j.jsg.2021.104386, 2021
Krýza, O., Zádava, P., and Lexa, O.: Advanced strain and mass
transfer analysis in crustal-scale oroclinal buckling and detachment folding
analogue models, Tectonophysics, 764, 88–109,
https://doi.org/10.1016/j.tecto.2019.05.001, 2019.
Ladd, C. R. and Reber, J. E.: The effect of a liquid phase on force
distribution during deformation in a granular system, J. Geophys. Res.-Solid
Ea., 125, e2020JB019771, https://doi.org/10.1029/2020JB019771, 2020.
Lamplugh, G. W.: Structure of the Weald and analogous tracts, Q. J. Geol.
Soc. Lond., 75, 73–95, 1919.
Lavier, L. L. and Manatschal, G.: A mechanism to thin the continental
lithosphere at magma-poor margins, Nature, 440, 324–328,
https://doi.org/10.1038/nature04608, 2006.
Lebinson, F., Turienzo, M., Sánchez, N., Cristallini, E., Arauja, V.,
and Dimieri, L.: Kinematics of a backthrust system in the Agrio fold and
thrust belt, T Argentina: Insights from structural analysis and analogue
models, J. S. Am. Earth Sci., 100, 102594,
https://doi.org/10.1016/j.jsames.2020.102594, 2020.
Lefeuvre, N., Truche, L., Donzeì, F.-V., Ducoux, M., Barreì, G.,
Fakoury, R.-A., Calassou, S., and Gaucher, E. C.: Native H2 Exploration in
the Western Pyrenean Foothills, Geochem. Geophy. Geosy., 22, e2021GC009917,
https://doi.org/10.1029/2021GC009917, 2021.
Lescoutre, R. and Manatschal, G.: Role of rift-inheritance and segmentation
for orogenic evolution: example from the Pyrenean-Cantabrian system, Bull.
Soc. Geol. Fr., 191, 18, https://doi.org/10.1051/bsgf/2020021, 2020.
Letouzey, J.: Fault reactivation, inversion and fold-thrust belt, in:
Petroleum and Tectonics in Mobile Belts, edited by Letouzey, J., Editions
Technip, Paris, France, 101–128, ISBN: 9782710805793, 1990.
Letouzey, J., Colletta, B., Vialy, R., and Chermetter, J. C.: Evolution of
salt-related structures in compressional settings, in: Salt tectonics, a
global perspective, edited by: Jackson, M. P. A., Roberts, D. G., and
Snelson, S., AAPG Memoir, 65, 41–60,
https://doi.org/10.1306/M65604C3, 1995.
Li, Z., Dong, M., Li, S., and Huang, S.: CO2 sequestration in depleted
oil and gas reservoirs – caprock characterization and storage capacity,
Energ. Convers. Manage., 47, 1372–1382,
https://doi.org/10.1016/j.enconman.2005.08.023, 2006.
Liang, P., Zhong, R., Zhao, L., and Xie, Y.: Formation of Fe-Cu-Au deposit
in basin inversion setting in NW China: A perspective from ore-fluid halogen
and noble gas geochemistry, Ore Geol. Rev., 131, 104011,
https://doi.org/10.1016/j.oregeorev.2021.104011, 2021.
Likerman, J., Burlando, J. F., Cristallini, E. O., and Ghiglione, M. C.:
Along-strike structural variations in the Southern Patagonian Andes:
Insights from physical modelling, Tectonophysics, 590, 106–120,
https://doi.org/10.1016/j.tecto.2013.01.018, 2013.
Lohrmann, J., Kukowski, N., Adam, J., and Oncken, O.: The impact of analogue
material properties on the geometry, kinematics, and dynamics of convergent
sand wedges, J. Struct. Geol., 25, 1691–1711,
https://doi.org/10.1016/S0191-8141(03)00005-1, 2003.
Lowell, J. D.: Plate Tectonics and Foreland Basement Deformation, Geology,
2, 275–278, https://doi.org/10.1130/0091-7613(1974)2<275:PTAFBD>2.0.CO;2, 1974.
Lowell, J. D.: Mechanics of basin inversion from worldwide examples, Geol.
Soc. Spec. Publ., 88, 39–57,
https://doi.org/10.1144/GSL.SP.1995.088.01.04, 1995.
Luth, S., Willingshofer, E., Sokoutis, D., and Cloetingh, S.: Analogue
modelling of continental collision: Influence of plate coupling on mantle
lithosphere subduction, crustal deformation and surface topography,
Tectonophysics, 484, 87–102,
https://doi.org/10.1016/j.tecto.2009.08.043, 2010.
Madritsch, H., Naef, H., Meier, B., Franzke, H. J., and Schreurs, G.:
Architecture and Kinematics of the Constance-Frick Trough (Northern
Switzerland): Implications for the Formation of Post-Variscan Basins in the
Foreland of the Alps and Scenarios of Their Neogene Reactivation, Tectonics,
37, 2197–2220, https://doi.org/10.1029/2017TC004945, 2018.
Maestrelli, D., Bonini, M., Corti, G., Del Ventisette, C., Moratti, G., and
Montanari, D.: Exploring fault propagation and the role of inherited
structures during caldera collapse through laboratory experiments, J.
Volcan. Geoth. Res., 414, 107232,
https://doi.org/10.1016/j.jvolgeores.2021.107232, 2021.
Maestrelli, D., Montanari, D., Corti, G., Del Ventisette, C., Moratti, G.,
and Bonini, M.: Exploring the Interactions Between Rift Propagation and
Inherited Crustal Fabrics Through Experimental Modeling, Tectonics, 39,
e2020TC006211, https://doi.org/10.1029/2020TC006211, 2020.
Maillot, B.: A sedimentation device to produce uniform sand packs,
Tectonophysics, 593, 85–94,
https://doi.org/10.1016/j.tecto.2013.02.028, 2013.
Mandal, N. and Chattopadhyay, A.: Modes of reverse reactivation of
domino-type normal faults: experimental and theoretical approach, J. Struct.
Geol., 17, 1151–1163,
https://doi.org/10.1016/0191-8141(95)00015-6, 1995.
Marques, F. O. and Nogueira, C. R.: Normal fault inversion by orthogonal
compression: Sandbox experiments with weak faults, J. Struct. Geol., 30,
761–766, https://doi.org/10.1016/j.jsg.2008.02.015, 2008.
Marques, F. O., Nogueira, F. C. C., Bezerra, F. H. R., and de Castro, D. L.:
The Araripe Basin in NE Brazil: An intracontinental graben inverted to a
high-standing horst, Tectonophysics, 630, 251–264,
https://doi.org/10.1016/j.tecto.2014.05.029, 2014.
Martínez, F. and Cristallini, E.: The doubly vergent inverted
structures in the Mesozoic basins of northern Chile (28∘ S): A
comparative analysis from field data and analogue modeling, J. S. Am. Earth
Sci., 77, 327–340,
https://doi.org/10.1016/j.jsames.2017.02.002, 2017.
Martínez, F., Bonini, M., Montanari, D., and Corti. G.: Tectonic
inversion and magmatism in the Lautaro Basin, northern Chile, Central Andes:
A comparative approach from field data and analog models, J. Geodyn., 94/95,
68–83, https://doi.org/10.1016/j.jog.2016.02.003, 2016.
Martínez, F., Montanari, D., Del Ventisette, C., and Bonini, M.: Basin
inversion and magma migration and emplacement: Insights from basins of
northern Chile, J. Struct. Geol., 114, 310–319,
https://doi.org/10.1016/j.jsg.2017.12.008, 2018.
Massaro, L., Adam, J., Jonade, E., and Yamada, Y.: New granular
rock-analogue materials for simulation of multi-scale fault and fracture
processes, Geol. Mag., 1–24,
https://doi.org/10.1017/S0016756821001321, 2021.
Mattioni, L., Sassi, W., and Callot, J.-P.: Analogue models of basin
inversion by transpression: role of structural heterogeneity, Geol. Soc.
London, Spec. Publ., 272, 397–417,
https://doi.org/10.1144/GSL.SP.2007.272.01.20, 2007.
Mayolle, S., Soliva, R., Dominguez, S., Wibberley, C., and Caniven, Y.:
Nonlinear fault damage zone scaling revealed through analog modelling,
Geology, 49, 968–972, https://doi.org/10.1130/G48760.1, 2021.
McClay, K. R.: Analogue models of inversion tectonics, Geol. Soc. Spec.
Publ., 44, 41–59,
https://doi.org/10.1144/GSL.SP.1989.044.01.04, 1989.
McClay, K. R.: Extensional fault systems in sedimentary basins: a review of
analogue model studies, Mar. Petrol. Geol., 7, 206–233,
https://doi.org/10.1016/0264-8172(90)90001-W, 1990.
McClay, K. R.: The geometries and kinematics of inverted fault systems: a
review of analogue modelling studies, Geol. Soc. Spec. Publ., 88, 97–118,
https://doi.org/10.1144/GSL.SP.1995.088.01.07, 1995.
McClay, K. R.: Recent advances in analogue modelling: uses in section
interpretation and validation, Geol. Soc. Spec. Publ., 99, 201–225,
https://doi.org/10.1144/GSL.SP.1996.099.01.16, 1996.
McClay, K. R. and Buchanan, P. G.: Thrust faults in inverted extensional
basin, in: Thrust Tectonics, edited by: McClay, K. R., Springer, Dordrecht, 93–104,
https://doi.org/10.1007/978-94-011-3066-0_8, 1992.
McClay, K. R., Dooley, T., Ferguson, A., and Poblet, J.: Tectonic Evolution
of the Sanga Sanga Block, Mahakam Delta, Kalimantan, Indonesia, AAPG Bull.,
84, 765–786,
https://doi.org/10.1306/A96733EC-1738-11D7-8645000102C1865D, 2000.
McClay, K., Dooley, T. P., Whitehouse, P., and Mills, M.: 4-D evolution of
rift systems: Insights from scaled physical models, Am. Assoc. Pet. Geol.
Bull., 86, 935–959,
https://doi.org/10.1306/61EEDBF2-173E-11D7-8645000102C1865D, 2002.
Mencos, J., Carrera, N., and Muñoz, J. A.: Influence of rift basin
geometry on the subsequent postrift sedimentation and basin inversion: The
Organyà Basin and the Bóixols thrust sheet (south central Pyrenees),
Tectonics, 35, 1452–1474, https://doi.org/10.1002/2014TC003692, 2015.
Michon, L. and Merle, O.: Crustal structures of the Rhinegraben and the
Massif Central grabens: An experimental approach, Tectonics, 19, 896–904,
https://doi.org/10.1029/2000TC900015, 2000.
Michon, L. and Merle, O.: Mode of lithospheric extension: Conceptual models
from analogue modeling, Tectonics, 22, 1028,
https://doi.org/10.1029/2002TC001435, 2003.
Miró, J., Ferrer, O., Muñoz, J. A., and Manastchal, G.: Role of inheritance during tectonic inversion of a rift system in a thick- to thin-skin transition: Analogue modelling and application to the Pyrenean – Biscay System, EGUsphere [preprint], https://doi.org/10.5194/egusphere-2022-1175, 2022.
Mitra, S.: Geometry and kinematic evolution of inversion structures, AAPG
Bull., 77, 1159–1191,
https://doi.org/10.1306/BDFF8E2A-1718-11D7-8645000102C1865D, 1993.
Mitra, S. and Islam, Q. T.: Experimental (clay) models of inversion
structures, Tectonophysics, 230, 211–222,
https://doi.org/10.1016/0040-1951(94)90136-8, 1994.
Mock, S. and Herwegh, M.: Tectonics of the central Swiss Molasse Basin:
Post-Miocene transition to incipient thick-skinned tectonics?, Tectonics,
36, 1699–1723, https://doi.org/10.1002/2017TC004584, 2017.
Molnar, N. E., Cruden, A. R., and Betts, P. G.: Interactions between
propagating rotational rifts and linear rheological heterogeneities:
Insights from three-dimensional laboratory experiments, Tectonics, 36,
420–443, https://doi.org/10.1002/2016TC004447, 2017.
Montanari, D., Agostini, A., Bonini, M., Corti, G., and Ventisette, C.: The
Use of Empirical Methods for Testing Granular Materials in Analogue
Modelling, Materials (Basel), 10, 635,
https://doi.org/10.3390/ma10060635, 2017.
Moretti, I. and Webber, M. E.: Natural hydrogen: a geological curiosity or
the primary energy source for a low-carbon future?, Renewable Matter,
https://www.renewablematter.eu/articles/article/ (last access: 20 October 2022), 2021.
Mourgues, R. and Cobbold, P. R.: Some tectonic consequences of fluid
overpressures and seepage forces as demonstrated by sandbox modelling,
Tectonophysics, 376, 75–97,
https://doi.org/10.1016/S0040-1951(03)00348-2, 2003.
Moragas, M., Vergés, J., Nalpas, T., Saura, E., Martín-Martín,
J. D., Message, G., and Hunt, D. W.: The impact of syn- and post-extension
prograding sedimentation on the development of salt-related rift basins and
their inversion: Clues from analogue modelling, Mar. Petrol. Geol., 88,
985–1003, https://doi.org/10.1016/j.marpetgeo.2017.10.001, 2017.
Morley, C. K.: Stress re-orientation along zones of weak fabrics in rifts:
An explanation for pure extension in “oblique” rift segments?, Earth Planet
Sc. Lett., 297, 667–673,
https://doi.org/10.1016/j.epsl.2010.07.022, 2010.
Moulas, E., Sokoutis, D., and Willingshofer, E.: Pressure build-up and
stress variations within the Earth's crust in the light of analogue models,
Sci. Rep., 9, 2310, https://doi.org/10.1038/s41598-018-38256-1, 2019.
Muñoz-Sáez, C., Pinto, L., Charrier, R., and Nalpas, T.: Influence
of depositional load on the development of a shortcut fault system during
the inversion of an extensional basin: The Eocene-Oligocene Abanico Basin
case, central Chile Andes (33∘–35∘ S), Andean Geol.,
41, 1–28, https://doi.org/10.5027/andgeoV41n1-a01, 2014.
Munteanu, I., Willingshofer, E., Sokoutis, D., Matenco, L., Dinu, C., and
Cloetingh, S.: Transfer of deformation in back-arc basins with a laterally
variable rheology: Constraints from analogue modelling of the
Balkanides–Western Black Sea inversion, Tectonophysics, 602, 223–236,
https://doi.org/10.1016/j.tecto.2013.03.009, 2013.
Munteanu, I., Willingshofer, E., Matenco, L., and Sokoutis, D.: Far-field
contractional polarity changes in models and nature, Earth Planet. Sc.
Lett., 395, 101–115,
https://doi.org/10.1016/j.epsl.2014.03.036, 2014.
Musso Piantelli, F., Mair, D., Berger, A., Schlunegger, F., Wiederkehr, M., Kurmann, E.,
Baumberger, R., Möri, A., and Herwegh, M.: 4D reconstruction of the Doldenhorn nappebasement
system in the Aar massif: Insights into late-stage continent-continent collision in the
Swiss Alps, Tectonophysics, 843, 229586, https://doi.org/10.1016/j.tecto.2022.229586, 2022.
Nalpas, T., Le Douaran, S., Brun, J.-P., Unternehr, P., and Richert, J.-P.:
Inversion of the Broad Fourteens Basin (offshore Netherlands), a small-scale
model investigation, Sediment. Geol., 95, 237–250,
https://doi.org/10.1016/0037-0738(94)00113-9, 1995.
Naylor, M. A., Laroque, J. M., and Gauthier. B. D. M.: Understanding
extensional tectonics: Insights from sandbox models, in: Geodynamic
Evolution of Sedimentary Basins, edited by: Roure, F., Ellouz, N., and Shein,
V. S., Skvortsov, International Symposium, Moscow, Editions Technip, Paris, France, 69–83, ISBN: 9782710806929, 1994.
Nestola, Y., Storti, F., Bedogni, E., and Cavozzi, C.: Shape evolution and
finite deformation pattern in analog experiments of lithosphere necking,
Geophys. Res. Lett., 40, 5025–5057,
https://doi.org/10.1002/grl.50978, 2013.
Nestola, Y., Storti, F., and Cavozzi, C.: Strain rate-dependent lithosphere
rifting and necking architectures in analog experiments, J. Geophys. Res.,
120, 584–594, https://doi.org/10.1002/2014JB011623, 2015.
Nieuwland, D. A., Urai, J. L., and Knoop, M.: In-situ stress measurements in
model experiments of tectonic faulting, in: Aspects of Tectonic Faulting,
edited by: Lehner, F. K., Urai, J. L., and Van der Zee, W., Springer-Verlag,
Berlin Heidelberg, https://doi.org/10.1007/978-3-642-59617-9_8, 2000.
Oertel, G.: The mechanism of faulting in clay experiments, Tectonophysics,
2, 343–393, https://doi.org/10.1016/0040-1951(65)90032-6, 1965.
Oriolo, S., Cristallini, E. O., Japas, M. S., and Yagupsky, D. L.: Neogene
structure of the Andean Precordillera, Argentina: insights from analogue
models, Andean Geol., 42, 20–35,
https://doi.org/10.5027/andgeoV42n1-a02, 2015.
Osagiede, E. E., Rosenau, M., Rotevatn, A., Gawthorpe, R., Jackson, C. A-L.,
and Rudolf, M.: Influence of zones of pre-existing crustal weakness on
strain localization and partitioning during rifting: Insights from analog
modeling using high-resolution 3D digital image correlation, Tectonics, 40,
e2021TC006970, https://doi.org/10.1029/2021TC006970, 2021.
Panien, M., Schreurs, G., and Pfiffner, A.: Sandbox experiments on basin
inversion: testing the influence of basin orientation and basin fill, J.
Struct. Geol., 27, 433–445,
https://doi.org/10.1016/j.jsg.2004.11.001, 2005.
Panien, M., Buiter, S. J. H., Schreurs, G., and Pfiffner, O. A.: Inversion
of a symmetric basin: insights from a comparison between analogue and
numerical experiments, Geol. Soc. Spec. Publ., 253, 253–270,
https://doi.org/10.1144/GSL.SP.2006.253.01.13, 2006a.
Panien, M., Schreurs, G., and Pfiffner, O. A.: Mechanical behaviour of
granular materials used in analogue modelling: insights from grain
characterisation, ring-shear tests and analogue experiments, J. Struct.
Geol., 28, 1710–1724,
https://doi.org/10.1016/j.jsg.2006.05.004, 2006b.
Park, Y., Kang, N., Yi, B., Lee, G., and Yoo, D.: Tectonostratigraphic
framework in the eastern Korean continental margin, East Sea: Implication
for evolution of the Hupo Basin, Basin Res., 34, 1–27,
https://doi.org/10.1111/bre.12641, 2021.
Payrola, P. A., Hongn, F., Cristallini, E., Carcía, V., and Del Papa,
C.: Andean oblique folds in the Cordillera Oriental – Northwestern
Argentina: Insights from analogue models, J. Struct. Geol., 42, 194–211,
https://doi.org/10.1016/j.jsg.2012.05.003, 2012.
Pfiffner, O. A.: The structure of the Helvetic nappes and its relation to
the mechanical stratigraphy, J. Struct, Geol., 15, 511–521,
https://doi.org/10.1016/0191-8141(93)90145-Z, 1993.
Philippe, Y.: Rampes Latérales et zones de transfert dans les
chaînes plissées: géométrie, conditions de formations et
pièges structuraux associés, Ph.D. Theses, Université de Savoie,
France, 351 pp., https://hal.archives-ouvertes.fr/tel-00755680/ (last access: 20 October 2022),
1995.
Philippon, M. and Corti, G.: Obliquity along plate boundaries,
Tectonophysics, 693, 171–182,
https://doi.org/10.1016/j.tecto.2016.05.033, 2016.
Pinto, L., Muñoz, C., Nalpas, T., and Charrier, R.: Role of
sedimentation during basin inversion in analogue modelling, J. Struct.
Geol., 32, 554–565, https://doi.org/10.1016/j.jsg.2010.03.001, 2010.
Plenefisch, T. and Bonjer, K.-P.: The stress field in the Rhine Graben area
inferred from earthquake focal mechanisms and estimation of frictional
parameters, Tectonophysics, 275, 71–97,
https://doi.org/10.1016/S0040-1951(97)00016-4, 1997.
Poppe, S., Holohan, E. P., Galland, O., Buls, N., Van Gompel, G., Keelson,
B., Tournigand, P.-Y., Brancart, J., Hollis, D., Nila, A., and Kervyn, M.:
An Inside Perspective on Magma Intrusion: Quantifying 3D Displacement and
Strain in Laboratory Experiments by Dynamic X-Ray Computed Tomography,
Front. Earth Sci., 7, 62,
https://doi.org/10.3389/feart.2019.00062, 2019.
Ramberg, H.: Gravity, Deformation and the Earth's Crust, Academic Press,
London, ISBN: 9780125768603, 1981.
Ranalli, G.: Experimental tectonics: from Sir James Hall to the present, J.
Geodyn., 32, 65–76,
https://doi.org/10.1016/S0264-3707(01)00023-0, 2001.
Reber, J. E., Cooke, M. L., and Dooley, T. P.: What model material to use? A
Review on rock analogs for structural geology and tectonics, Earth-Sci.
Rev., 202, 103107,
https://doi.org/10.1016/j.earscirev.2020.103107, 2020.
Reitano, R., Faccenna, C., Funiciello, F., Corbi, F., and Willett, S. D.:
Erosional response of granular material in landscape models, Earth Surf.
Dynam., 8, 973–993, https://doi.org/10.5194/esurf-8-973-2020, 2020.
Reitano, R., Faccenna, C., Funiciello, F., Corbi, F., Sternai P., Willett,
S. D., Sembroni A., and Lanari R.: Sediment recycling and the evolution of
analogue orogenic wedges, Tectonics, 42, e2021TC006951,
https://doi.org/10.1029/2021TC006951, 2022.
Richard, P.: Champs de failles au dessus d'un décrochement de socle:
modélisation expérimentale, Memoires et documents du Centre
Armoricain d'Etude Structurale des Socles, 34, PhD Thesis, Université
Rennes 1, https://tel.archives-ouvertes.fr/tel-00675425
(last access: 20 October 2022), 1989.
Richetti, P. C., Zwaan, F., Schreurs, G., Schmitt, R. S., and Schmid, T. C.: Analogue modelling of basin inversion: the role of oblique kinematics and implications for the Araripe Basin (Brazil), EGUsphere [preprint], https://doi.org/10.5194/egusphere-2022-1251, 2022.
Rincón, M., Márquez, A., Herrera, R., Galland, O., Sánchez-Oro,
J., Concha, D., and Monemayor, A. S.: Monitoring volcanic and tectonic
sandbox analogue models using the Kinect v2 sensor, Earth Space Sci., 9,
e2020EA001368, https://doi.org/10.1029/2020EA001368, 2020.
Ritter, M. C., Leever, K. A., Rosenau, M., and Oncken, O.: Scaling the
sandbox – Mechanical (dis) similarities of granular materials and brittle
rock, J. Geophys. Res.-Sol. Ea, 121, 6863–6879,
https://doi.org/10.1002/2016JB012915, 2016.
Ritter, M. C., Leever, K. A., Rosenau, M., and Oncken, O.: Growing Faults in
the Lab: Insights Into the Scale Dependence of the Fault Zone Evolution
Process, Tectonics, 37, 140–153,
https://doi.org/10.1002/2017TC004787, 2018a.
Ritter, M. C., Santimano, T., Rosenau, M., Leever, K. A., and Oncken, O.:
Sandbox rheometry: Co-evolution of stress and strain in Riedel – and
Critical Wedge–experiments, Tectonophysics, 722, 400–409,
https://doi.org/10.1016/j.tecto.2017.11.018, 2018b.
Roma, M., Ferrer, O., McClay, K. R., Muñoz, J. A., Roca, E.,
Gratacós, O., and Cabello, P.: Weld kinematics of syn-rift salt during
basement-involved extension and subsequent inversion: Results from analog
models, Geol. Acta, 16, 391–410,
https://doi.org/10.1344/GeologicaActa2018.16.4.4, 2018a.
Roma. M., Vidal-Royo, O., McClay, K., Ferrer, O., and Muñoz, J. A.:
Tectonic inversion of salt-detachment ramp-syncline basins as illustrated by
analog modeling and kinematic restoration, Interpretation, 6, 1F-T229,
https://doi.org/10.1190/INT-2017-0073.1, 2018b.
Roscoe, K. H.: The influence of strains in soil mechanics, 10th Rankine
Lecture, Geotechnique, 20, 129–170,
https://doi.org/10.1680/geot.1970.20.2.129, 1970.
Rosenau, M., Lohrmann, J., and Oncken, O.: Shocks in a box: An analogue
model of subduction earthquake cycles with application to seismotectonic
forearc evolution, J. Geophys. Res., 114, 1–20,
https://doi.org/10.1029/2008JB005665, 2009.
Roure, F. and Colletta, B.: Cenozoic inversion structures in the foreland of
the Pyrenees and Alps, in: Peri-Tethys Memoir 2: Structure and Prospects of
Alpine Basins and Forelands, edited by: Ziegler, P. A. and Horvàth, F.,
Mémoires du Muséum national d'histoire naturelle, Muséum national d’histoire naturelle, 170, 173–209, ISBN: 2-85653-507-0,
https://www.biodiversitylibrary.org/page/58832613 (last access: 20 October 2022), 1996.
Rudolf, M., Boutelier, D., Rosenau, M., Schreurs, G., and Oncken, O.:
Rheological benchmark of silicone oils used for analog modeling of short-
and long-term lithospheric deformation, Tectonophysics, 684, 12–22,
https://doi.org/10.1016/j.tecto.2015.11.028, 2016.
Rudolf, M., Rosenau, M., and Oncken, O.: Time dependent properties of
granular media – The GeoMod Benchmark 2021, GeoMod 2021, Doorn,
Netherlands, 19–23 September 2021,
https://geomod2021.uu.nl/wp-content/uploads/sites/512/2021/09/Abstract-volume-GeoMod-2021-2.pdf (last access: 20 October 2022), 2021.
Ruh, J. B.: Effects of fault-weakening processes on oblique intracontinental
rifting and subsequent tectonic inversion, Am. J. Sci., 319, 315–338,
https://doi.org/10.2475/04.2019.03, 2019.
Ruh, J. B. and Vergés, J.: Effects of reactivated extensional basement
faults on structural evolution of fold-and-thrust belts: Insights from
numerical modelling applied to the Kopet Dagh Mountains, Tectonophysics,
746, 493–511, https://doi.org/10.1016/j.tecto.2017.05.020, 2018.
Sandiford, M.: Mechanics of basin inversion, Tectonophysics, 305, 109–120,
https://doi.org/10.1016/S0040-1951(99)00023-2, 1999.
Sanford, A. R.: Analytical and experimental study of simple geological
studies, GSA Bull., 70, 19–52,
https://doi.org/10.1130/0016-7606(1959)70[19:AAESOS]2.0.CO;2, 1959.
Sani, F., Del Ventisette, C., Montanari, D., Bendkik, A., and Chenakeb, M.:
Structural evolution of the Rides Prerifaines (Morocco): structural and
seismic interpretation and analogue modelling experiments, Int. J. Earth.
Sci., 96, 685–706, https://doi.org/10.1007/s00531-006-0118-2, 2007.
Santimano, T. and Pyskluwec, R.: The influence of lithospheric mantle scars
and rheology on intraplate deformation and orogenesis: Insights from
tectonic analog models, Tectonics, 39, e2019TC005841,
https://doi.org/10.1029/2019TC005841, 2020.
Saria, E., Calais, E., Stamps, D. S., Delvaux, D., and Hartnady, C. J. H.:
Present-day kinematics of the East African Rift, J. Geophys. Res.-Sol. Ea.,
119, 3584–3600, https://doi.org/10.1002/2013JB010901, 2014.
Sassi, W., Colletta, B., Balé, P., and Paquereau, T.: Modelling of
structural complexity in sedimentary basins: the role of pre-existing faults
in thrust tectonics, Tectonophysics, 226, 97–112,
https://doi.org/10.1016/0040-1951(93)90113-X, 1993.
Schellart, W. P.: Shear test results for cohesion and friction coefficients
for different granular materials: scaling implications for their usage in
analogue modelling, Tectonophysics, 324, 1–16,
https://doi.org/10.1016/S0040-1951(00)00111-6, 2000.
Schellart, W. P. and Strak, V.: A review of analogue modelling of geodynamic
processes: Approaches, scaling, materials and quantification, with an
application to subduction experiments, J. Geodyn., 100, 7–32,
https://doi.org/10.1016/j.jog.2016.03.009, 2016.
Schmid, S., Kissling, E., Diehl, T., Van Hindsbergen, D., and Molli, G.:
Ivrea mantle wedge, arc of the Western Alps, and kinematic evolution of the
Alps–Apennines orogenic system, Swiss, J. Geosci., 110, 581–612,
https://doi.org/10.1007/s00015-016-0237-0, 2017.
Schmid, T., Schreurs, G., Warsitzka, M., and Rosenau, M.: Effect of sieving
height on density and friction of brittle analogue material: Ring-shear test
data of quarz sand used for analogue experiments in the Tectonic Modelling
Lab of the University of Bern, GFZ Data Services [data set],
https://doi.org/10.5880/fidgeo.2020.006, 2020.
Schmid, T. C., Schreurs, G., and Adam, J.: Characteristics of continental
rifting in rotational systems: New findings from spatiotemporal high
resolution quantified crustal scale analogue models, Tectonophysics, 822,
229174, https://doi.org/10.1016/j.tecto.2021.229174, 2022.
Schöfisch, T., Koyi, H., and Almqvist, B.: Infuence of décollement
friction on anisotropy of magnetic susceptibility in a fold-and-thrust belt
model, J. Struct. Geol., 144, 104274,
https://doi.org/10.1016/j.jsg.2020.104274, 2021.
Schori, M., Zwaan, F., Schreurs, G., and Mosar, J.: Pre-existing Basement
Faults Controlling Deformation in the Jura Mountains Fold-and-Thrust Belt:
Insights from Analogue Models, Tectonophysics, 814, 228980,
https://doi.org/10.1016/j.tecto.2021.228980, 2021.
Schreurs, G. and Colletta, B.: Analogue modelling of faulting in zones of
continental transpression and transtension, Geol. Soc. Spec. Publ., 135,
59–79, https://doi.org/10.1144/GSL.SP.1998.135.01.05, 1998.
Schreurs, G., Hänni, R., Panien, M., and Vock, P.: Analysis of analogue
models by helical X-ray computed tomography, Geol Soc. Spec. Publ., 2015,
213–223, https://doi.org/10.1144/GSL.SP.2003.215.01.20, 2003.
Schreurs, G., Buiter, S. J. H., Boutelier, D., Corti, G., Costa, E., Cruden,
A. R., Daniel, J.-M., Hoth, S., Koyi, H. A., Kukowski, N., Lohrmann, J.,
Ravaglia, A., Schlische, R. W., Withjack, M. O., Yamada, Y., Cavozzi, C.,
Del Ventisette, C., Brady, J. A. E., Hoffmann-Rothe, A., Mengus, J.-M.,
Montanari, D., and Nilfouroushan, F.: Analogue benchmarks of shortening and
extension experiments, Geol. Soc. Lond. Spec. Publ., 253, 1–27,
https://doi.org/10.1144/GSL.SP.2006.253.01.01, 2006.
Schreurs, G., Buiter, S. J. H., Boutelier, J., Burberry, C., Callot, J.-P.,
Cavozzi, C., Cerca, M., Chen, J.-H., Cristallini, E., Cruden, A. R., Cruz,
L., Daniel, J.-M., Da Poian, G., Garcia, V. H., Gomes, C. J. S., Grall, C.,
Guillot, Y., Guzmán, C., Hidayah, T. N., Hilley, G. E., Klinkmüller,
M., Koyi, H. A., Lu, C.-Y., Maillot, B., Meriaux, C., Nilfouroushan, F.,
Pan, C.-C., Pillot, D., Portillo, R., Rosenau, M., Schellart, W. P.,
Schlische, R. W., Take, A., Vendeville, B., Vergnaud, M., Vettori, M., Wang,
S.-H., Withjack, M. O., Yagupsky, D., and Yamada, Y.: Benchmarking analogue
models of brittle thrust wedges, J. Struct. Geol., 92, 116–139.
https://doi.org/10.1016/j.jsg.2016.03.005, 2016.
Scott, E.: Exploring for native hydrogen, Nature Rev. Earth Environ., 2,
589, https://doi.org/10.1038/s43017-021-00215-2, 2021.
Sibuet, J.-C., Srivastava, S. P., and Spakman, W.: Pyrenean orogeny and
plate kinematics, J. Geophys. Res., 109, B08104,
https://doi.org/10.1029/2003JB002514, 2004.
Sibson, R. H.: A note on fault reactivation, J. Struct. Geol., 7, 751–754,
https://doi.org/10.1016/0191-8141(85)90150-6, 1985.
Sibson, R. H.: Selective fault reactivation during basin inversion:
potential for fluid redistribution through fault-valve action, Geol. Soc.
Spec. Publ., 88, 3–19,
https://doi.org/10.1144/GSL.SP.1995.088.01.02, 1995.
Sibson, R. H.: Rupturing in overpressured crust during compressional
inversion – the case from NE Honshu, Japan, Tectonophysics, 473, 404–416,
https://doi.org/10.1016/j.tecto.2009.03.016, 2009.
Sibson, R. H. and Scott, J.: Stress/fault controls on the containment and
release of overpressured fluids: Examples from gold–quartz vein systems in
Juneau, Alaska; Victoria, Australia and Otago, New Zealand, Ore Geol. Rev.,
13, 293–306, https://doi.org/10.1016/S0169-1368(97)00023-1, 1998.
Smith, N. J. P.: It's time for explorationists to take hydrogen more
seriously, First Break, 20, 246–253, 2002.
Sokoutis, D. and Willingshofer, E.: Decoupling during continental collision
and intra-plate deformation, Earth Planet. Sc. Lett., 305, 435–444,
https://doi.org/10.1016/j.epsl.2011.03.028, 2011.
Souloumiac, P., Maillot, B., and Leroy, Y. M.: Bias due to side wall
friction in sand box experiments, J. Struct. Geol., 35, 90–101,
https://doi.org/10.1016/j.jsg.2011.11.002, 2012.
Souriot, T. and Brun, J.-P.: Faulting and block rotation in the Afar
triangle, East Africa: the Danakil “crank-arm” model., Geology, 20,
911–914, https://doi.org/10.1130/0091-7613, 1992.
Stewart, S. A.: Salt tectonics in the North Sea Basin: a structural style
template for seismic interpreters, Geol. Soc. Spec. Publ., 272, 361–396,
https://doi.org/10.1144/GSL.SP.2007.272.01.19, 2007.
Stewart, S. A. and Clark, J. A.: Impact of salt on the structure of the
Central North Sea hydrocarbon fairways, Petrol. Geol. Conf. Ser., 5,
179–200, https://doi.org/10.1144/0050179, 1999.
Stewart, S. A. and Coward, M. P.: Synthesis of salt tectonics in the
southern North Sea, UK, Mar. Petrol. Geol., 12, 457–475,
https://doi.org/10.1016/0264-8172(95)91502-G, 1995.
Strzerzynski, P., Dominguez, S., Boudial, A., and Déverchère, J.:
Tectonic inversion and geomorphic evolution of the Algerian margin since
Messinian times: Insights from new onshore/offshore analog modeling
experiments, Tectonics, 40, e2020TC006369.
https://doi.org/10.1029/2020TC006369, 2021.
Tron, V. and Brun, J.-P.: Experiments on oblique rifting in brittle-ductile
systems, Tectonophysics, 188, 71–84,
https://doi.org/10.1016/0040-1951(91)90315-J, 1991.
Tari, G., Arbouille, D., Schléder, Z., and Tóth, T.: Inversion
tectonics: a brief petroleum industry perspective, Solid Earth, 11,
1865–1889, https://doi.org/10.5194/se-11-1865-2020, 2020.
Turner, J. P. and Williams, G. A.: Sedimentary basin inversion and intra-plate
shortening, Earth-Sci. Rev., 65, 277–304,
https://doi.org/10.1016/j.earscirev.2003.10.002, 2004.
Ustaszewski, K., Schumacher, M. E., Schmid, S. M., and Nieuwland, D.: Fault
reactivation in brittle–viscous wrench systems–dynamically scaled analogue
models and application to the Rhine–Bresse transfer zone, Quaternary Sci.
Rev., 24, 365–382,
https://doi.org/10.1016/j.quascirev.2004.03.015, 2005.
Van Winden, M., De Jager, J., Jaarsma, B., and Bouroullec, R.: New insights
into salt tectonics in the northern Dutch offshore: a framework for
hydrocarbon exploration, Geol Soc. Spec. Publ., 469, 99–117,
https://doi.org/10.1144/SP469.9, 2018.
Vaughan, A. P. M. and Scarrow, J. H.: Ophiolite obduction pulses as a proxy
indicator of superplume events?, Earth Planet. Sc. Lett., 213, 407–416,
https://doi.org/10.1016/S0012-821X(03)00330-3, 2003.
Vendeville, B., Cobbold, P. R., Davy, P., Brun, J.-P., and Choukroune, P.:
Physical models of extensional tectonics at various scales, Geol Soc. Spec.
Publ., 28, 95–107,
https://doi.org/10.1144/GSL.SP.1987.028.01.08, 1987.
Vermeer, P. A.: The orientation of shear bands in biaxial tests,
Géotechnique, 40, 223–236,
https://doi.org/10.1680/geot.1990.40.2.223, 1990.
Vially, R., Letouzey, J., Bénard, F., Haddadi N., Desforges, G., Askari,
H., and Boujema, A.: Basin inversion along the North African Margin – The
Saharan Atlas (Algeria), in: Peri-Tethyan Platforms, edited by: Roure, F.,
Editions Technip, Paris, France, 79–118, ISBN: 9782710806790, 1994.
Vidal, J. and Genter, A.: Overview of naturally permeable fractured
reservoirs in the central and southern Upper Rhine Graben: Insights from
geothermal wells, Geothermics, 74, 57–73,
https://doi.org/10.1016/j.geothermics.2018.02.003, 2018.
Villarroel, M., Jara, P., Herrera, S., and Charrier, R.: In uence of the
orientation of cohesive blocks upon the structural grain of fold-and-thrust
belts: An appraisal by means of analogue modeling, J. S. Am. Earth. Sci.,
103, 102725, https://doi.org/10.1016/j.jsames.2020.102725, 2020.
Voormeij, D. A. and Simandl, G. J.: Geological, ocean, and mineral CO2
sequestration options: A technical review, Geosci. Can., 31, 11–22, 2004.
Wang, Q., Li, S., Guo, L., Suo. Y., and Dai., L.: Analogue modelling and
mechanism of tectonic inversion of the Xihu Sag, East China Sea Shelf Basin,
J. Asian Earth Sci., 139, 129–141,
https://doi.org/10.1016/j.jseaes.2017.01.026, 2017.
Warren J. K.: Flowing Salt: Halokinesis, in: Evaporites, edited by: Warren,
J.K., Springer, Cham, 491–612,
https://doi.org/10.1007/978-3-319-13512-0_6, 2016.
Weibel, R., Olivarius, M., Vosgerau H., Mathiesen, A., Kristensen, L.,
Nielsen, C., and Nielsen, L.: Overview of potential geothermal reservoirs in
Denmark, Neth. J. Geosci., 99, E3,
https://doi.org/10.1017/njg.2020.5, 2020.
Weijermars, R.: Flow behaviour and physical chemistry of bouncing putties
and related polymers in view of tectonic laboratory applications,
Tectonophysics, 124, 325–358,
https://doi.org/10.1016/0040-1951(86)90208-8, 1986.
Weijermars, R. and Schmeling, H.: Scaling of Newtonian and non-Newtonian
fluid dynamics without inertia for quantitative modelling of rock flow due
to gravity (including the concept of rheological similarity), Phys. Earth
Planet. In., 43, 316–330,
https://doi.org/10.1016/0031-9201(86)90021-X, 1986.
Willems, C. J. L., Vondrak, A., Mijnlief, H. F., Donselaar, M. E., and Van
Kempen, B. M. M.: Geology of the Upper Jurassic to Lower Cretaceous
geothermal aquifers in the West Netherlands Basin – an overview, Neth. J.
Geosci., 99, E1, https://doi.org/10.1017/njg.2020.1, 2020.
Williams, G. D., Powell, C. M., and Cooper, M. A.: Geometry and kinematics
of inversion tectonics, Geol. Soc. Spec. Publ., 44, 3–15,
https://doi.org/10.1144/gsl.sp.1989.044.01.02, 1989.
Willingshofer, E. and Sokoutis, D.: Decoupling along plate boundaries: Key
variable controlling the mode of deformation and the geometry of collisional
mountain belts, Geology, 37, 39–42,
https://doi.org/10.1130/G25321A.1, 2009.
Willingshofer, E., Sokoutis, D., Luth, S. W., Beekman, F., and Cloetingh,
S.: Subduction and deformation of the continental lithosphere in response to
plate and crust-mantle coupling, Geology, 41, 1239–1242,
https://doi.org/10.1130/G34815.1, 2013.
Wilson, R. W., Houseman, G. A., Buiter, S. J. H., McCaffrey, K. J. W., and
Doré, A. G.: Fifty years of the Wilson Cycle concept in plate tectonics:
an overview, Geol. Soc. Spec. Publ., 470, 1–17,
https://doi.org/10.1144/SP470-2019-58, 2019.
Withjack, M. O. and Callaway, S.: Active normal faulting beneath a salt
layer: An experimental study of deformation patterns in the cover sequence,
AAPG Bull., 84, 627–651,
https://doi.org/10.1306/C9EBCE73-1735-11D7-8645000102C1865D, 2000.
Withjack, M. O. and Jamison, W. R.: Deformation produced by oblique rifting,
Tectonophysics, 126, 99–124,
https://doi.org/10.1016/0040-1951(86)90222-2, 1986.
Yagupsky, D. L., Cristallini, E. O., Fantín, J., Valcarce, G. Z.,
Bottesi, G., and Varadé, R.: Oblique half-graben inversion of the
Mesozoic Neuquén Rift in the Malargüe Fold and Thrust Belt, Mendoza,
Argentina: New insights from analogue models, J. Struct. Geol., 30, 839–853,
https://doi.org/10.1016/j.jsg.2008.03.007, 2008.
Yamada, Y. and McClay, K. R.: Application of geometric models to inverted
listric fault systems in sandbox experiments. Paper 1: 2D hanging wall
deformation and section restoration, J. Struct. Geol., 25, 1551–1560,
https://doi.org/10.1016/S0191-8141(02)00181-5, 2003a.
Yamada, Y. and McClay, K. R.: Application of geometric models to inverted
listric fault systems in sandbox experiments, Paper 2: insights for possible
along strike migration of material during 3D hanging wall deformation, J.
Struct. Geol., 25, 1331–1336,
https://doi.org/10.1016/S0191-8141(02)00160-8, 2003b.
Yamada, Y. and McClay, K. R.: 3-D analogue modeling of inversion thrust
structures, in: Thrust tectonics and hydrocarbon systems, edited by: McClay,
K. R., AAPG Memoir, 82, 276–301,
https://doi.org/10.1306/M82813C16, 2004.
Yamada, Y. and McClay, K. R.: Influence of shear angle on hangingwall
deformation during tectonic inversion, Isl. Arc, 19, 546–559,
https://doi.org/10.1111/j.1440-1738.2010.00731.x, 2010.
Yu, F., Zhang, R., Yu, J., Wang, Y., Chen, S., Liu, J., Wu, C., Wang, Y.,
Wang, S., Wang, Y., and Liu, Y.: Meso-Cenozoic negative inversion model for
the Linhe Depression of Hetao Basin, China, Geol. Mag., 1–24,
https://doi.org/10.1017/S0016756821001138, 2021.
Ziegler, P. A., Cloetingh, S., and Van Wees, J.-D.: Dynamics of intra-plate
compressional deformation: the Alpine foreland and other examples,
Tectonophysics, 252, 7–59,
https://doi.org/10.1016/0040-1951(95)00102-6, 1995.
Zwaan, F. and Schreurs, G.: Rift segment interaction in orthogonal and
rotational extension experiments: Implications for the large-scale
development of rift systems, J. Struct. Geol., 140, 104119,
https://doi.org/10.1016/j.jsg.2020.104119, 2020.
Zwaan, F. and Schreurs, G.: Analogue Modeling of Continental Rifting: An
Overview, in: Continental Rifted Margins I, edited by: Peron-Pinvidic, G.,
ISTE-Wiley, https://doi.org/10.1002/9781119986928.ch6, 2022a.
Zwaan, F. and Schreurs, G.: Analogue models of lithospheric-scale rifting
monitored in an X-ray CT scanner, ESSOAr [preprint],
https://doi.org/10.1002/essoar.10510709.1, 2022b.
Zwaan, F., Schreurs, G., Naliboff, J., and Buiter, S. J. H.: Insights into
the effects of oblique extension on continental rift interaction from 3-D
analogue and numerical models, Tectonophysics, 693, 239–260,
https://doi.org/10.1016/j.tecto.2016.02.036, 2016.
Zwaan, F., Schreurs, G., and Adam, J.: Effects of sedimentation on rift
segment evolution and rift interaction in orthogonal and oblique extensional
settings: Insights from analogue models analysed with 4D X-ray computed
tomography and digital volume correlation techniques, Glob. Planet. Change,
171, 110–133, https://doi.org/10.1016/j.gloplacha.2017.11.002, 2018a.
Zwaan, F., Schreurs, G., Ritter, M., Santimano, T., and Rosenau, M.:
Rheology of PDMS-corundum sand mixtures from the Tectonic Modelling Lab of
the University of Bern (CH), V. 1. GFZ Data Services [data set],
https://doi.org/10.5880/fidgeo.2018.023, 2018b.
Zwaan, F., Schreurs, G., and Buiter, S. J. H.: A systematic comparison of
experimental set-ups for modelling extensional tectonics, Solid Earth, 10,
1063–1097, https://doi.org/10.5194/se-10-1063-2019, 2019.
Zwaan, F., Corti, G., Keir, D., and Sani, F.: Analogue modelling of marginal
flexure in Afar, East Africa: Implications for passive margin formation,
Tectonophysics, 796, 228595,
https://doi.org/10.1016/j.tecto.2020.228595, 2020a.
Zwaan, F., Schreurs, G., and Rosenau, M.: Rift propagation in rotational
versus orthogonal extension: Insights from 4D analogue models, J. Struct.
Geol., 135, 103946, https://doi.org/10.1016/j.jsg.2019.103946, 2020b.
Zwaan, F., Chenin, P., Erratt, D., Manatschal, G., and Schreurs, G.: Complex rift patterns, a result of interacting crustal and mantle weaknesses, or multiphase rifting? Insights from analogue models, Solid Earth, 12, 1473–1495, https://doi.org/10.5194/se-12-1473-2021, 2021.
Zwaan, F., Chenin, P., Erratt, D., Manatschal, G., and Scheurs, G.:
Competition between 3D structural inheritance and kinematics during rifting:
insights from analogue models, Basin Res., 34, 1–31,
https://doi.org/10.1111/bre.12642, 2022.
Short summary
When a sedimentary basin is subjected to compressional tectonic forces after its formation, it may be inverted. A thorough understanding of such
basin inversionis of great importance for scientific, societal, and economic reasons, and analogue tectonic models form a key part of our efforts to study these processes. We review the advances in the field of basin inversion modelling, showing how the modelling results can be applied, and we identify promising venues for future research.
When a sedimentary basin is subjected to compressional tectonic forces after its formation, it...
Special issue