Articles | Volume 14, issue 7
https://doi.org/10.5194/se-14-709-2023
© Author(s) 2023. 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-14-709-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
12 Jul 2023
Research article |
| 12 Jul 2023
| 12 Jul 2023
Inversion of accommodation zones in salt-bearing extensional systems: insights from analog modeling
Elizabeth Parker Wilson
CORRESPONDING AUTHOR
Institut de Recera Geomodels, Departament de Dinàmica de la Terra i de l'Oceà, Universitat de Barcelona, 08028, Barcelona, Spain
Pablo Granado
Institut de Recera Geomodels, Departament de Dinàmica de la Terra i de l'Oceà, Universitat de Barcelona, 08028, Barcelona, Spain
Pablo Santolaria
Institut de Recera Geomodels, Departament de Dinàmica de la Terra i de l'Oceà, Universitat de Barcelona, 08028, Barcelona, Spain
Oriol Ferrer
Institut de Recera Geomodels, Departament de Dinàmica de la Terra i de l'Oceà, Universitat de Barcelona, 08028, Barcelona, Spain
Josep Anton Muñoz
Institut de Recera Geomodels, Departament de Dinàmica de la Terra i de l'Oceà, Universitat de Barcelona, 08028, Barcelona, Spain
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Pablo Santolaria, Roi Silva-Casal, Núria Carrera, Josep A. Muñoz, Pau Arbués, and Pablo Granado
EGUsphere, https://doi.org/10.5194/egusphere-2025-1742, https://doi.org/10.5194/egusphere-2025-1742, 2025
This preprint is open for discussion and under review for Solid Earth (SE).
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Among sedimentary rocks, evaporites (as salt) have a particular behavior when deformed under geological forces: they flow while the others break. Such behavior controls the evolution of mountain building events. By mapping the distribution of rocks and interpreting the subsurface architecture of geological structures we were able to reconstruct the mountain building processes of an area in the Southern Pyrenees and how those evaporites flowed and accumulated where we find them nowadays.
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
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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.
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
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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.
Frank Zwaan, Guido Schreurs, Susanne J. H. Buiter, Oriol Ferrer, Riccardo Reitano, Michael Rudolf, and Ernst Willingshofer
Solid Earth, 13, 1859–1905, https://doi.org/10.5194/se-13-1859-2022, https://doi.org/10.5194/se-13-1859-2022, 2022
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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.
Stefano Tavani, Pablo Granado, Amerigo Corradetti, Thomas Seers, Josep Maria Casas, and Josep Anton Muñoz
Solid Earth, 11, 1643–1651, https://doi.org/10.5194/se-11-1643-2020, https://doi.org/10.5194/se-11-1643-2020, 2020
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Using orthophotos, we manually digitized 30 000 joints in the eastern Ebro Basin of the Pyrenees. Joints are perpendicular to the belt in the frontal portion of the belt and in the inner and central portion of the foredeep basin. Joint orientations in the external portion of the foredeep become less clustered. Joints in the studied area formed in the foredeep in response to foredeep-parallel stretching, which becomes progressively less intense within the external portion of the foredeep basin.
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
Stefano Tavani, Pablo Granado, Pau Arbués, Amerigo Corradetti, and J. Anton Muñoz
Solid Earth, 8, 405–419, https://doi.org/10.5194/se-8-405-2017, https://doi.org/10.5194/se-8-405-2017, 2017
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In the the Sant Corneli-Bóixols anticline, a syn-growth unconformity divides and de-couples a lower overturned pre-growth unit from an upper syn-growth one. Pre-growth strata and the unconformity underwent syn-folding shearing, even where they are mutually perpendicular. Different and coeval shear senses occurring at different structural positions indicate that regardless of its orientation, layering in the pre- and syn-growth sequences of the anticline was continuously sheared.
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: Structural geology
Lithologically constrained velocity–density relationships and vertical stress gradients in the North Alpine Foreland Basin, SE Germany
Unbiased statistical length analysis of linear features: adapting survival analysis to geological applications
Earthquake swarms frozen in an exhumed hydrothermal system (Bolfin Fault Zone, Chile)
Reconciling post-orogenic faulting, paleostress evolution, and structural inheritance in the seismogenic northern Apennines (Italy): insights from the Monti Martani Fault System
Understanding the stress field at the lateral termination of a thrust fold using generic geomechanical models and clustering methods
Localized shear and distributed strain accumulation as competing shear accommodation mechanisms in crustal shear zones: constraining their dictating factors
Strike-slip kinematics from crustal to outcrop-scale: the impact of the material properties on the analogue modelling
Influence of water on crystallographic preferred orientation patterns in a naturally deformed quartzite
Geomorphic expressions of active rifting reflect the role of structural inheritance: a new model for the evolution of the Shanxi Rift, northern China
The Size Distributions of Faults and Earthquakes: Implications for Orogen-Internal Seismogenic Deformation
Poro-perm relations of Mesozoic carbonates and fault breccia, Araxos Promontory, NW Greece
Driven magmatism and crustal thinning of coastal southern China in response to subduction
Selection and characterization of the target fault for fluid-induced activation and earthquake rupture experiments
Naturally fractured reservoir characterisation in heterogeneous sandstones: insight for uranium in situ recovery (Imouraren, Niger)
Multiscalar 3D temporal structural characterisation of Smøla island, mid-Norwegian passive margin: an analogue for unravelling the tectonic history of offshore basement highs
Impact of faults on the remote stress state
Subduction plate interface shear stress associated with rapid subduction at deep slow earthquake depths: example from the Sanbagawa belt, southwestern Japan
Multiple phase rifting and subsequent inversion in the West Netherlands Basin: implications for geothermal reservoir characterization
Analogue modelling of basin inversion: implications for the Araripe Basin (Brazil)
Natural fracture patterns at Swift Reservoir anticline, NW Montana: the influence of structural position and lithology from multiple observation scales
Rapid hydration and weakening of anhydrite under stress: implications for natural hydration in the Earth's crust and mantle
Analogue experiments on releasing and restraining bends and their application to the study of the Barents Shear Margin
Structural framework and timing of the Pahtohavare Cu ± Au deposits, Kiruna mining district, Sweden
Does the syn- versus post-rift thickness ratio have an impact on the inversion-related structural style?
Structural control of inherited salt structures during inversion of a domino basement-fault system from an analogue modelling approach
Kinematics and time-resolved evolution of the main thrust-sense shear zone in the Eo-Alpine orogenic wedge (the Vinschgau Shear Zone, eastern Alps)
Role of inheritance during tectonic inversion of a rift system in basement-involved to salt-decoupled transition: analogue modelling and application to the Pyrenean–Biscay system
Water release and homogenization by dynamic recrystallization of quartz
Hydrothermal activity of the Lake Abhe geothermal field (Djibouti): Structural controls and paths for further exploration
Time-dependent frictional properties of granular materials used in analogue modelling: implications for mimicking fault healing during reactivation and inversion
Large grain-size-dependent rheology contrasts of halite at low differential stress: evidence from microstructural study of naturally deformed gneissic Zechstein 2 rock salt (Kristallbrockensalz) from the northern Netherlands
Analogue modelling of the inversion of multiple extensional basins in foreland fold-and-thrust belts
A contribution to the quantification of crustal shortening and kinematics of deformation across the Western Andes ( ∼ 20–22° S)
Rift thermal inheritance in the SW Alps (France): insights from RSCM thermometry and 1D thermal numerical modelling
The Luangwa Rift Active Fault Database and fault reactivation along the southwestern branch of the East African Rift
Clustering has a meaning: optimization of angular similarity to detect 3D geometric anomalies in geological terrains
Shear zone evolution and the path of earthquake rupture
Mechanical compaction mechanisms in the input sediments of the Sumatra subduction complex – insights from microstructural analysis of cores from IODP Expedition 362
Detecting micro fractures: a comprehensive comparison of conventional and machine-learning-based segmentation methods
Multiscale lineament analysis and permeability heterogeneity of fractured crystalline basement blocks
Structural characterization and K–Ar illite dating of reactivated, complex and heterogeneous fault zones: lessons from the Zuccale Fault, Northern Apennines
How do differences in interpreting seismic images affect estimates of geological slip rates?
Progressive veining during peridotite carbonation: insights from listvenites in Hole BT1B, Samail ophiolite (Oman)
Tectonic evolution of the Indio Hills segment of the San Andreas fault in southern California, southwestern USA
Structural diagenesis in ultra-deep tight sandstones in the Kuqa Depression, Tarim Basin, China
Variscan structures and their control on latest to post-Variscan basin architecture: insights from the westernmost Bohemian Massif and southeastern Germany
Multi-disciplinary characterizations of the BedrettoLab – a new underground geoscience research facility
Biotite supports long-range diffusive transport in dissolution–precipitation creep in halite through small porosity fluctuations
De-risking the energy transition by quantifying the uncertainties in fault stability
Virtual field trip to the Esla Nappe (Cantabrian Zone, NW Spain): delivering traditional geological mapping skills remotely using real data
Peter Obermeier, Florian Duschl, and Michael C. Drews
Solid Earth, 16, 425–440, https://doi.org/10.5194/se-16-425-2025, https://doi.org/10.5194/se-16-425-2025, 2025
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We investigate geophysical properties and the distribution of vertical stress, which is defined by the weight of the rock column above a certain location in the subsurface, in the upper 5 km of the North Alpine Foreland Basin in Germany. Our results help us to understand the present-day geological configuration and to improve safety for subsurface use, such as deep geothermal energy production in the study area.
Gabriele Benedetti, Stefano Casiraghi, Daniela Bertacchi, and Andrea Bistacchi
Solid Earth, 16, 367–390, https://doi.org/10.5194/se-16-367-2025, https://doi.org/10.5194/se-16-367-2025, 2025
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At any scale, the limited size of a study area introduces a bias in the interpretation of linear features, defined as right-censoring bias. We show the effects of not considering such bias and apply survival analysis techniques to obtain unbiased estimates of multiple parametrical distributions in three censored length datasets. Finally, we propose a novel approach to select the most representative model from a sensible candidate pool using the probability integral transform technique.
Simone Masoch, Giorgio Pennacchioni, Michele Fondriest, Rodrigo Gomila, Piero Poli, José Cembrano, and Giulio Di Toro
Solid Earth, 16, 23–43, https://doi.org/10.5194/se-16-23-2025, https://doi.org/10.5194/se-16-23-2025, 2025
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We investigate an exhumed hydrothermal system in the Atacama Desert (Chile) to understand how earthquake swarms form. Wall rocks near fault veins experienced high-stress pulses, and fault veins underwent cyclic crack opening and shearing. These findings suggest ancient earthquake swarm activity, from dynamic crack propagation to repeated crack opening and shearing. This system represents a unique geological record of earthquake swarms, providing insights into their initiation and evolution.
Riccardo Asti, Selina Bonini, Giulio Viola, and Gianluca Vignaroli
Solid Earth, 15, 1525–1551, https://doi.org/10.5194/se-15-1525-2024, https://doi.org/10.5194/se-15-1525-2024, 2024
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This study addresses the tectonic evolution of the seismogenic Monti Martani Fault System (northern Apennines, Italy). By applying a field-based structural geology approach, we reconstruct the evolution of the stress field and we challenge the current interpretation of the fault system in terms of both geometry and state of activity. We stress that the peculiar behavior of this system during post-orogenic extension is still significantly influenced by the pre-orogenic structural template.
Anthony Adwan, Bertrand Maillot, Pauline Souloumiac, Christophe Barnes, Christophe Nussbaum, Meinert Rahn, and Thomas Van Stiphout
Solid Earth, 15, 1445–1463, https://doi.org/10.5194/se-15-1445-2024, https://doi.org/10.5194/se-15-1445-2024, 2024
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We use computer simulations to study how stress is distributed in large-scale geological models, focusing on how fault lines behave under pressure. By running many 2D and 3D simulations with varying conditions, we discover patterns in how faults form and interact. Our findings reveal that even small changes in conditions can lead to different stress outcomes. This research helps us better understand earthquake mechanics and could improve predictions of fault behavior in real-world scenarios.
Pramit Chatterjee, Arnab Roy, and Nibir Mandal
Solid Earth, 15, 1281–1301, https://doi.org/10.5194/se-15-1281-2024, https://doi.org/10.5194/se-15-1281-2024, 2024
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Understanding strain accumulation processes in shear zones is essential for explaining failure mechanisms at great crustal depths. This study explores the rheological and kinematic factors determining the varying modes of shear accommodation in natural shear zones. Numerical simulations suggest that an interplay of parameters – initial viscosity, bulk shear rate, and internal cohesion – governs the dominance of one accommodation mechanism over another.
Luigi Massaro, Jürgen Adam, Elham Jonade, Silvia Negrão, and Yasuhiro Yamada
EGUsphere, https://doi.org/10.5194/egusphere-2024-3116, https://doi.org/10.5194/egusphere-2024-3116, 2024
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In this manuscript, we investigated the kinematics and dynamics of strike-slip damage zones using laboratory mechanical tests and analogue modelling techniques. The results underline the importance of a multi-scale approach (from crustal to outcrop-scale) to improve the understanding of such deformation processes, deriving fundamental correlations with the physical and mechanical properties of the model materials applied in the experiments.
Jeffrey M. Rahl, Brendan Moehringer, Kenneth S. Befus, and John S. Singleton
Solid Earth, 15, 1233–1240, https://doi.org/10.5194/se-15-1233-2024, https://doi.org/10.5194/se-15-1233-2024, 2024
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At the high temperatures present in the deeper crust, minerals such as quartz can flow much like silly putty. The detailed mechanisms of how atoms are reorganized depends upon several factors, such as the temperature and the rate of which the mineral changes shape. We present observations from a naturally deformed rock showing that the amount of water present also influences the type of deformation in quartz, with implications for geological interpretations.
Malte Froemchen, Ken J. W. McCaffrey, Mark B. Allen, Jeroen van Hunen, Thomas B. Phillips, and Yueren Xu
Solid Earth, 15, 1203–1231, https://doi.org/10.5194/se-15-1203-2024, https://doi.org/10.5194/se-15-1203-2024, 2024
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The Shanxi Rift is a young, active rift in northern China that formed atop a Proterozoic orogen. The impact of these structures on active rift faults is poorly understood. Here, we quantify the landscape response to active faulting and compare it with published maps of inherited structures. We find that inherited structures played an important role in the segmentation of the Shanxi Rift and in the development of rift interaction zones, which are the most active regions in the Shanxi Rift.
Sandro Truttmann, Tobias Diehl, Marco Herwegh, and Stefan Wiemer
EGUsphere, https://doi.org/10.5194/egusphere-2024-2975, https://doi.org/10.5194/egusphere-2024-2975, 2024
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Our study investigates the statistical relationship between geological faults and earthquakes in the Southwestern Swiss Alps. We analyze how the fault size and earthquake rupture are related and find differences in how faults at different depths rupture seismically. While shallow faults tend to rupture only partially, deeper faults are more likely to rupture along their entire length, potentially resulting in larger earthquakes.
Sergio C. Vinciguerra, Federico Vagnon, Irene Bottero, Jerome Fortin, Angela Vita Petrullo, Dimitrios Spanos, Aristotelis Pagoulatos, and Fabrizio Agosta
EGUsphere, https://doi.org/10.5194/egusphere-2024-2823, https://doi.org/10.5194/egusphere-2024-2823, 2024
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We assessed the poro-perm relations of both host rocks and fault rocks of Mesozoic carbonate rocks, by integrating a laboratory petrophysical studyn with a digital image analysis. Three different protocols were employed to compute permeability: i) Effective Medium Theory on laboratory data, ii) constant crack aperture and iii) crack density values from 2D images. Carbonate host rocks did not show a clear poro-perm trend due to the presence of stiff, sub-rounded pores and of small vugs.
Jinbao Su, Wenbin Zhu, and Guangwei Li
Solid Earth, 15, 1133–1141, https://doi.org/10.5194/se-15-1133-2024, https://doi.org/10.5194/se-15-1133-2024, 2024
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The late Mesozoic igneous rocks in the South China Block exhibit flare-ups and lulls, which form in compressional or extensional backgrounds. The ascending of magma forms a mush-like head and decreases crustal thickness. The presence of faults and pre-existing magmas will accelerate emplacement of underplating magma. The magmatism at different times may be formed under similar subduction conditions, and the boundary compression forces will delay magma ascent.
Peter Achtziger-Zupančič, Alberto Ceccato, Alba Simona Zappone, Giacomo Pozzi, Alexis Shakas, Florian Amann, Whitney Maria Behr, Daniel Escallon Botero, Domenico Giardini, Marian Hertrich, Mohammadreza Jalali, Xiaodong Ma, Men-Andrin Meier, Julian Osten, Stefan Wiemer, and Massimo Cocco
Solid Earth, 15, 1087–1112, https://doi.org/10.5194/se-15-1087-2024, https://doi.org/10.5194/se-15-1087-2024, 2024
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We detail the selection and characterization of a fault zone for earthquake experiments in the Fault Activation and Earthquake Ruptures (FEAR) project at the Bedretto Lab. FEAR, which studies earthquake processes, overcame data collection challenges near faults. The fault zone in Rotondo granite was selected based on geometry, monitorability, and hydro-mechanical properties. Remote sensing, borehole logging, and geological mapping were used to create a 3D model for precise monitoring.
Maxime Jamet, Gregory Ballas, Roger Soliva, Olivier Gerbeaud, Thierry Lefebvre, Christine Leredde, and Didier Loggia
Solid Earth, 15, 895–920, https://doi.org/10.5194/se-15-895-2024, https://doi.org/10.5194/se-15-895-2024, 2024
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This study characterizes the Tchirezrine II sandstone reservoir in northern Niger. Crucial for potential uranium in situ recovery (ISR), our multifaceted approach reveals (i) a network of homogeneously distributed orthogonal structures, (ii) the impact of clustered E–W fault structures on anisotropic fluid flow, and (iii) local changes in the matrix behaviour of the reservoir as a function of the density and nature of the deformation structure.
Matthew S. Hodge, Guri Venvik, Jochen Knies, Roelant van der Lelij, Jasmin Schönenberger, Øystein Nordgulen, Marco Brönner, Aziz Nasuti, and Giulio Viola
Solid Earth, 15, 589–615, https://doi.org/10.5194/se-15-589-2024, https://doi.org/10.5194/se-15-589-2024, 2024
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Smøla island, in the mid-Norwegian margin, has complex fracture and fault patterns resulting from tectonic activity. This study uses a multiple-method approach to unravel Smøla's tectonic history. We found five different phases of deformation related to various fracture geometries and minerals dating back hundreds of millions of years. 3D models of these features visualise these structures in space. This approach may help us to understand offshore oil and gas reservoirs hosted in the basement.
Karsten Reiter, Oliver Heidbach, and Moritz O. Ziegler
Solid Earth, 15, 305–327, https://doi.org/10.5194/se-15-305-2024, https://doi.org/10.5194/se-15-305-2024, 2024
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It is generally assumed that faults have an influence on the stress state of the Earth’s crust. It is questionable whether this influence is still present far away from a fault. Simple numerical models were used to investigate the extent of the influence of faults on the stress state. Several models with different fault representations were investigated. The stress fluctuations further away from the fault (> 1 km) are very small.
Yukinojo Koyama, Simon R. Wallis, and Takayoshi Nagaya
Solid Earth, 15, 143–166, https://doi.org/10.5194/se-15-143-2024, https://doi.org/10.5194/se-15-143-2024, 2024
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Stress along a subduction plate boundary is important for understanding subduction phenomena such as earthquakes. We estimated paleo-stress using quartz recrystallized grain size combined with deformation temperature and P–T paths of exhumed rocks. The obtained results show differential stresses of 30.8–82.7 MPa consistent over depths of 17–27 km in the paleo-subduction boundary. The obtained stress may represent the initial conditions under which slow earthquakes nucleated in the same domain.
Annelotte Weert, Kei Ogata, Francesco Vinci, Coen Leo, Giovanni Bertotti, Jerome Amory, and Stefano Tavani
Solid Earth, 15, 121–141, https://doi.org/10.5194/se-15-121-2024, https://doi.org/10.5194/se-15-121-2024, 2024
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On the road to a sustainable planet, geothermal energy is considered one of the main substitutes when it comes to heating. The geological history of an area can have a major influence on the application of these geothermal systems, as demonstrated in the West Netherlands Basin. Here, multiple episodes of rifting and subsequent basin inversion have controlled the distribution of the reservoir rocks, thus influencing the locations where geothermal energy can be exploited.
Pâmela C. Richetti, Frank Zwaan, Guido Schreurs, Renata S. Schmitt, and Timothy C. Schmid
Solid Earth, 14, 1245–1266, https://doi.org/10.5194/se-14-1245-2023, https://doi.org/10.5194/se-14-1245-2023, 2023
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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 1000 m height, allowing for studies thereof, 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.
Adam J. Cawood, Hannah Watkins, Clare E. Bond, Marian J. Warren, and Mark A. Cooper
Solid Earth, 14, 1005–1030, https://doi.org/10.5194/se-14-1005-2023, https://doi.org/10.5194/se-14-1005-2023, 2023
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Here we test conceptual models of fracture development by investigating fractures across multiple scales. We find that most fractures increase in abundance towards the fold hinge, and we interpret these as being fold related. Other fractures at the site show inconsistent orientations and are unrelated to fold formation. Our results show that predicting fracture patterns requires the consideration of multiple geologic variables.
Johanna Heeb, David Healy, Nicholas E. Timms, and Enrique Gomez-Rivas
Solid Earth, 14, 985–1003, https://doi.org/10.5194/se-14-985-2023, https://doi.org/10.5194/se-14-985-2023, 2023
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Hydration of rocks is a key process in the Earth’s crust and mantle that is accompanied by changes in physical traits and mechanical behaviour of rocks. This study assesses the influence of stress on hydration reaction kinetics and mechanics in experiments on anhydrite. We show that hydration occurs readily under stress and results in localized hydration along fractures and mechanic weakening. New gypsum growth is selective and depends on the stress field and host anhydrite crystal orientation.
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
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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.
Leslie Logan, Ervin Veress, Joel B. H. Andersson, Olof Martinsson, and Tobias E. Bauer
Solid Earth, 14, 763–784, https://doi.org/10.5194/se-14-763-2023, https://doi.org/10.5194/se-14-763-2023, 2023
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The Pahtohavare Cu ± Au deposits in the Kiruna mining district have a dubious timing of formation and have not been contextualized within an up-to-date tectonic framework. Structural mapping was carried out to reveal that the deposits are hosted in brittle structures that cut a noncylindrical, SE-plunging anticline constrained to have formed during the late-Svecokarelian orogeny. These results show that Cu ± Au mineralization formed more than ca. 80 Myr after iron oxide–apatite mineralization.
Alexandra Tamas, Dan M. Tamas, Gabor Tari, Csaba Krezsek, Alexandru Lapadat, and Zsolt Schleder
Solid Earth, 14, 741–761, https://doi.org/10.5194/se-14-741-2023, https://doi.org/10.5194/se-14-741-2023, 2023
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Tectonic processes are complex and often difficult to understand due to the limitations of surface or subsurface data. One such process is inversion tectonics, which means that an area initially developed in an extension (such as the opening of an ocean) is reversed to compression (the process leading to mountain building). In this research, we use a laboratory method (analogue modelling), and with the help of a sandbox, we try to better understand structures (folds/faults) related to inversion.
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
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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.
Chiara Montemagni, Stefano Zanchetta, Martina Rocca, Igor M. Villa, Corrado Morelli, Volkmar Mair, and Andrea Zanchi
Solid Earth, 14, 551–570, https://doi.org/10.5194/se-14-551-2023, https://doi.org/10.5194/se-14-551-2023, 2023
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The Vinschgau Shear Zone (VSZ) is one of the largest and most significant shear zones developed within the Late Cretaceous thrust stack in the Austroalpine domain of the eastern Alps. 40Ar / 39Ar geochronology constrains the activity of the VSZ between 97 and 80 Ma. The decreasing vorticity towards the core of the shear zone, coupled with the younging of mylonites, points to a shear thinning behavior. The deepest units of the Eo-Alpine orogenic wedge were exhumed along the VSZ.
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
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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.
Junichi Fukuda, Takamoto Okudaira, and Yukiko Ohtomo
Solid Earth, 14, 409–424, https://doi.org/10.5194/se-14-409-2023, https://doi.org/10.5194/se-14-409-2023, 2023
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We measured water distributions in deformed quartz by infrared spectroscopy mapping and used the results to discuss changes in water distribution resulting from textural development. Because of the grain size reduction process (dynamic recrystallization), water contents decrease from 40–1750 wt ppm in host grains of ~2 mm to 100–510 wt ppm in recrystallized regions composed of fine grains of ~10 µm. Our results indicate that water is released and homogenized by dynamic recrystallization.
Bastien Walter, Yves Géraud, Alexiane Favier, Nadjib Chibati, and Marc Diraison
EGUsphere, https://doi.org/10.5194/egusphere-2023-397, https://doi.org/10.5194/egusphere-2023-397, 2023
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Lake Abhe in southwestern Djibouti is known for its exposures of massive hydrothermal chimneys and hot springs on the lake’s eastern shore. This study highlights the control of the main structural faults of the area on the development of these hydrothermal features. This work contributes to better understand hydrothermal fluid pathways in this area and may help further exploration for the geothermal development of this remarkable site.
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
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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.
Jessica Barabasch, Joyce Schmatz, Jop Klaver, Alexander Schwedt, and Janos L. Urai
Solid Earth, 14, 271–291, https://doi.org/10.5194/se-14-271-2023, https://doi.org/10.5194/se-14-271-2023, 2023
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We analysed Zechstein salt with microscopes and observed specific microstructures that indicate much faster deformation in rock salt with fine halite grains when compared to salt with larger grains. This is important because people build large cavities in the subsurface salt for energy storage or want to deposit radioactive waste inside it. When engineers and scientists use grain-size data and equations that include this mechanism, it will help to make better predictions in geological models.
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
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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.
Tania Habel, Martine Simoes, Robin Lacassin, Daniel Carrizo, and German Aguilar
Solid Earth, 14, 17–42, https://doi.org/10.5194/se-14-17-2023, https://doi.org/10.5194/se-14-17-2023, 2023
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The Central Andes are one of the most emblematic reliefs on Earth, but their western flank remains understudied. Here we explore two rare key sites in the hostile conditions of the Atacama desert to build cross-sections, quantify crustal shortening, and discuss the timing of this deformation at ∼20–22°S. We propose that the structures of the Western Andes accommodated significant crustal shortening here, but only during the earliest stages of mountain building.
Naïm Célini, Frédéric Mouthereau, Abdeltif Lahfid, Claude Gout, and Jean-Paul Callot
Solid Earth, 14, 1–16, https://doi.org/10.5194/se-14-1-2023, https://doi.org/10.5194/se-14-1-2023, 2023
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We investigate the peak temperature of sedimentary rocks of the SW Alps (France), using Raman spectroscopy on carbonaceous material. This method provides an estimate of the peak temperature achieved by organic-rich rocks. To determine the timing and the tectonic context of the origin of these temperatures we use 1D thermal modelling. We find that the high temperatures up to 300 °C were achieved during precollisional extensional events, not during tectonic burial in the Western Alps.
Luke N. J. Wedmore, Tess Turner, Juliet Biggs, Jack N. Williams, Henry M. Sichingabula, Christine Kabumbu, and Kawawa Banda
Solid Earth, 13, 1731–1753, https://doi.org/10.5194/se-13-1731-2022, https://doi.org/10.5194/se-13-1731-2022, 2022
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Mapping and compiling the attributes of faults capable of hosting earthquakes are important for the next generation of seismic hazard assessment. We document 18 active faults in the Luangwa Rift, Zambia, in an active fault database. These faults are between 9 and 207 km long offset Quaternary sediments, have scarps up to ~30 m high, and are capable of hosting earthquakes from Mw 5.8 to 8.1. We associate the Molaza Fault with surface ruptures from two unattributed M 6+ 20th century earthquakes.
Michał P. Michalak, Lesław Teper, Florian Wellmann, Jerzy Żaba, Krzysztof Gaidzik, Marcin Kostur, Yuriy P. Maystrenko, and Paulina Leonowicz
Solid Earth, 13, 1697–1720, https://doi.org/10.5194/se-13-1697-2022, https://doi.org/10.5194/se-13-1697-2022, 2022
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When characterizing geological/geophysical surfaces, various geometric attributes are calculated, such as dip angle (1D) or dip direction (2D). However, the boundaries between specific values may be subjective and without optimization significance, resulting from using default color palletes. This study proposes minimizing cosine distance among within-cluster observations to detect 3D anomalies. Our results suggest that the method holds promise for identification of megacylinders or megacones.
Erik M. Young, Christie D. Rowe, and James D. Kirkpatrick
Solid Earth, 13, 1607–1629, https://doi.org/10.5194/se-13-1607-2022, https://doi.org/10.5194/se-13-1607-2022, 2022
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Studying how earthquakes spread deep within the faults they originate from is crucial to improving our understanding of the earthquake process. We mapped preserved ancient earthquake surfaces that are now exposed in South Africa and studied their relationship with the shape and type of rocks surrounding them. We determined that these surfaces are not random and are instead associated with specific kinds of rocks and that their shape is linked to the evolution of the faults in which they occur.
Sivaji Lahiri, Kitty L. Milliken, Peter Vrolijk, Guillaume Desbois, and Janos L. Urai
Solid Earth, 13, 1513–1539, https://doi.org/10.5194/se-13-1513-2022, https://doi.org/10.5194/se-13-1513-2022, 2022
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Understanding the mechanism of mechanical compaction is important. Previous studies on mechanical compaction were mostly done by performing experiments. Studies on natural rocks are rare due to compositional heterogeneity of the sedimentary succession with depth. Due to remarkable similarity in composition and grain size, the Sumatra subduction complex provides a unique opportunity to study the micromechanism of mechanical compaction on natural samples.
Dongwon Lee, Nikolaos Karadimitriou, Matthias Ruf, and Holger Steeb
Solid Earth, 13, 1475–1494, https://doi.org/10.5194/se-13-1475-2022, https://doi.org/10.5194/se-13-1475-2022, 2022
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This research article focuses on filtering and segmentation methods employed in high-resolution µXRCT studies for crystalline rocks, bearing fractures, or fracture networks, of very small aperture. Specifically, we focus on the identification of artificially induced (via quenching) fractures in Carrara marble samples. Results from the same dataset from all five different methods adopted were produced and compared with each other in terms of their output quality and time efficiency.
Alberto Ceccato, Giulia Tartaglia, Marco Antonellini, and Giulio Viola
Solid Earth, 13, 1431–1453, https://doi.org/10.5194/se-13-1431-2022, https://doi.org/10.5194/se-13-1431-2022, 2022
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The Earth's surface is commonly characterized by the occurrence of fractures, which can be mapped, and their can be geometry quantified on digital representations of the surface at different scales of observation. Here we present a series of analytical and statistical tools, which can aid the quantification of fracture spatial distribution at different scales. In doing so, we can improve our understanding of how fracture geometry and geology affect fluid flow within the fractured Earth crust.
Giulio Viola, Giovanni Musumeci, Francesco Mazzarini, Lorenzo Tavazzani, Manuel Curzi, Espen Torgersen, Roelant van der Lelij, and Luca Aldega
Solid Earth, 13, 1327–1351, https://doi.org/10.5194/se-13-1327-2022, https://doi.org/10.5194/se-13-1327-2022, 2022
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A structural-geochronological approach helps to unravel the Zuccale Fault's architecture. By mapping its internal structure and dating some of its fault rocks, we constrained a deformation history lasting 20 Myr starting at ca. 22 Ma. Such long activity is recorded by now tightly juxtaposed brittle structural facies, i.e. different types of fault rocks. Our results also have implications on the regional evolution of the northern Apennines, of which the Zuccale Fault is an important structure.
Wan-Lin Hu
Solid Earth, 13, 1281–1290, https://doi.org/10.5194/se-13-1281-2022, https://doi.org/10.5194/se-13-1281-2022, 2022
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Having a seismic image is generally expected to enable us to better determine fault geometry and thus estimate geological slip rates accurately. However, the process of interpreting seismic images may introduce unintended uncertainties, which have not yet been widely discussed. Here, a case of a shear fault-bend fold in the frontal Himalaya is used to demonstrate how differences in interpretations can affect the following estimates of slip rates and dependent conclusions.
Manuel D. Menzel, Janos L. Urai, Estibalitz Ukar, Thierry Decrausaz, and Marguerite Godard
Solid Earth, 13, 1191–1218, https://doi.org/10.5194/se-13-1191-2022, https://doi.org/10.5194/se-13-1191-2022, 2022
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Mantle rocks can bind large quantities of carbon by reaction with CO2, but this capacity requires fluid pathways not to be clogged by carbonate. We studied mantle rocks from Oman to understand the mechanisms allowing their transformation into carbonate and quartz. Using advanced imaging techniques, we show that abundant veins were essential fluid pathways driving the reaction. Our results show that tectonic stress was important for fracture opening and a key ingredient for carbon fixation.
Jean-Baptiste P. Koehl, Steffen G. Bergh, and Arthur G. Sylvester
Solid Earth, 13, 1169–1190, https://doi.org/10.5194/se-13-1169-2022, https://doi.org/10.5194/se-13-1169-2022, 2022
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The San Andreas fault is a major active fault associated with ongoing earthquake sequences in southern California. The present study investigates the development of the Indio Hills area in the Coachella Valley along the main San Andreas fault and the Indio Hills fault. The Indio Hills area is located near an area with high ongoing earthquake activity (Brawley seismic zone), and, therefore, its recent tectonic evolution has implications for earthquake prediction.
Jin Lai, Dong Li, Yong Ai, Hongkun Liu, Deyang Cai, Kangjun Chen, Yuqiang Xie, and Guiwen Wang
Solid Earth, 13, 975–1002, https://doi.org/10.5194/se-13-975-2022, https://doi.org/10.5194/se-13-975-2022, 2022
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(1) Structural diagenesis analysis is performed on the ultra-deep tight sandstone. (2) Fracture and intergranular pores are related to the low in situ stress magnitudes. (3) Dissolution is associated with the presence of fracture.
Hamed Fazlikhani, Wolfgang Bauer, and Harald Stollhofen
Solid Earth, 13, 393–416, https://doi.org/10.5194/se-13-393-2022, https://doi.org/10.5194/se-13-393-2022, 2022
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Interpretation of newly acquired FRANKEN 2D seismic survey data in southeeastern Germany shows that upper Paleozoic low-grade metasedimentary rocks and possible nappe units are transported by Variscan shear zones to ca. 65 km west of the Franconian Fault System (FFS). We show that the locations of post-Variscan upper Carboniferous–Permian normal faults and associated graben and half-graben basins are controlled by the geometry of underlying Variscan shear zones.
Xiaodong Ma, Marian Hertrich, Florian Amann, Kai Bröker, Nima Gholizadeh Doonechaly, Valentin Gischig, Rebecca Hochreutener, Philipp Kästli, Hannes Krietsch, Michèle Marti, Barbara Nägeli, Morteza Nejati, Anne Obermann, Katrin Plenkers, Antonio P. Rinaldi, Alexis Shakas, Linus Villiger, Quinn Wenning, Alba Zappone, Falko Bethmann, Raymi Castilla, Francisco Seberto, Peter Meier, Thomas Driesner, Simon Loew, Hansruedi Maurer, Martin O. Saar, Stefan Wiemer, and Domenico Giardini
Solid Earth, 13, 301–322, https://doi.org/10.5194/se-13-301-2022, https://doi.org/10.5194/se-13-301-2022, 2022
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Questions on issues such as anthropogenic earthquakes and deep geothermal energy developments require a better understanding of the fractured rock. Experiments conducted at reduced scales but with higher-resolution observations can shed some light. To this end, the BedrettoLab was recently established in an existing tunnel in Ticino, Switzerland, with preliminary efforts to characterize realistic rock mass behavior at the hectometer scale.
Berit Schwichtenberg, Florian Fusseis, Ian B. Butler, and Edward Andò
Solid Earth, 13, 41–64, https://doi.org/10.5194/se-13-41-2022, https://doi.org/10.5194/se-13-41-2022, 2022
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Hydraulic rock properties such as porosity and permeability are relevant factors that have an impact on groundwater resources, geological repositories and fossil fuel reservoirs. We investigate the influence of chemical compaction upon the porosity evolution in salt–biotite mixtures and related transport length scales by conducting laboratory experiments in combination with 4-D analysis. Our observations invite a renewed discussion of the effect of sheet silicates on chemical compaction.
David Healy and Stephen Paul Hicks
Solid Earth, 13, 15–39, https://doi.org/10.5194/se-13-15-2022, https://doi.org/10.5194/se-13-15-2022, 2022
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The energy transition requires operations in faulted rocks. To manage the technical challenges and public concern over possible induced earthquakes, we need to quantify the risks. We calculate the probability of fault slip based on uncertain inputs, stresses, fluid pressures, and the mechanical properties of rocks in fault zones. Our examples highlight the specific gaps in our knowledge. Citizen science projects could produce useful data and include the public in the discussions about hazards.
Manuel I. de Paz-Álvarez, Thomas G. Blenkinsop, David M. Buchs, George E. Gibbons, and Lesley Cherns
Solid Earth, 13, 1–14, https://doi.org/10.5194/se-13-1-2022, https://doi.org/10.5194/se-13-1-2022, 2022
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We describe a virtual geological mapping course implemented in response to travelling and social restrictions derived from the ongoing COVID-19 pandemic. The course was designed to replicate a physical mapping exercise as closely as possible with the aid of real field data and photographs collected by the authors during previous years in the Cantabrian Zone (NW Spain). The course is delivered through Google Earth via a KMZ file with outcrop descriptions and links to GitHub-hosted photographs.
Cited articles
Adam, J., Urai, J. L., Wieneke, B., Oncken, O., Pfeiffer, K., Kukowski, N.,
Lohrmann, J., Hoth, S., van der Zee, W., and Schmatz, 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.
Ahlrichs, N., Hübscher, C., Noack, V., Schnabel, M., Damm, V., and
Krawczyk, C. M.: Structural Evolution at the Northeast North German Basin
Margin: From Initial Triassic Salt Movement to Late Cretaceous-Cenozoic
Remobilization, Tectonics, 39, e2019TC005927, https://doi.org/10.1029/2019TC005927, 2020.
Alves, T. M., Gawthorpe, R. L., Hunt, D. W., and Monteiro, J. H.: Jurassic
tectono-sedimentary evolution of the Northern Lusitanian Basin (offshore
Portugal), Mar. Petrol. Geol., 19, 727–754,
https://doi.org/10.1016/S0264-8172(02)00036-3, 2002.
Alves, T. M., Mattos, N. H., Newnes, S., and Goodall, S.: Analysis of a
basement fault zone with geothermal potential in the Southern North Sea,
Geothermics, 102, 102398, https://doi.org/10.1016/J.GEOTHERMICS.2022.102398,
2022.
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, 2005.
Beauchamp, W.: Superposed folding resulting from inversion of a synrift
accommodation zone, Atlas Mountains; Morocco, in: Thrust tectonics and
hydrocarbon systems, edited by: McClay, K. R., American Association of
Petroleum Geologists, 635–646, https://doi.org/10.1306/m82813c33, 2004.
Bonini, M.: Deformation patterns and structural vergence in brittle–ductile
thrust wedges: An additional analogue modelling perspective, J. Struct. Geol.,
29, 141–158, https://doi.org/10.1016/J.JSG.2006.06.012, 2007.
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.
Brun, J. P. and Fort, X.: Compressional salt tectonics (Angolan margin), Tectonophysics, 382, 129–150, https://doi.org/10.1016/j.tecto.2003.11.014, 2004.
Brun, J. P. and Nalpas, T.: Graben inversion in nature and experiments, Tectonics, 15, 677–687, https://doi.org/10.1029/95TC03853, 1996.
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, P. G. and McClay, K. R.: Experiments on basin inversion above
reactivated domino faults, Mar. Petrol. Geol., 9, 486–500,
https://doi.org/10.1016/0264-8172(92)90061-I, 1992.
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, Geological Society, London, Special Publications, 363, 395–408, https://doi.org/10.1144/SP363.18, 2012.
Callot, J. P., Trocmé,V., Letouzey, J., Albouy, E., Jahani, S., and Sherkati, S.: Pre-existing salt structures and the folding of the Zagros Mountains, Geological Society, London, Special Publications, 363, 545–561,
https://doi.org/10.1144/SP363.27, 2012.
Cartwright, J. A., Trudgill, B. D., and Mansfield, C. S.: Fault growth by segment
linkage: an explanation for scatter in maximum displacement and trace length
data from the Canyonlands Grabens of SE Utah, J. Struct. Geol.,
17, 1319–1326, 1995.
Célini, N., Callot, J. P., Ringenbach, J. C., and Graham, R.: Jurassic
salt tectonics in the SW sub-Alpine fold-and-thrust belt, Tectonics, 39,
e2020TC006107, https://doi.org/10.1029/2020TC006107, 2020.
Chapple, W.: Mechanics of thin-skinned fold-and-thrust belts, Am. Assoc. Pet.
Geol. Bull., 89, 1189–1198, https://doi.org/10.1130/0016-7606(1978)89<1189:MOTFB>2.0.CO;2, 1978.
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.
Costa, E. and Vendeville, B. C.: Experimental insights on the geometry and
kinematics of fold-and-thrust belts above weak, viscous evaporitic
décollement, J. Struct. Geol., 24, 1729–1739, 2002.
Coward, M. P.: Structural and tectonic setting of the Permo-Triassic basins
of northwest Europe, Geol. Soc. Spec. Publ., 91, 7–39,
https://doi.org/10.1144/GSL.SP.1995.091.01.02, 1995.
Crameri, F.: Geodynamic diagnostics, scientific visualisation and StagLab 3.0, Geosci. Model Dev., 11, 2541–2562, https://doi.org/10.5194/gmd-11-2541-2018, 2018.
Crameri, F., Shephard, G. E., and Heron, P. J.: The misuse of colour in
science communication, Nat. Commun., 11, 5444,
https://doi.org/10.1038/s41467-020-19160-7, 2020.
Davis, D. M. and Engelder, T.: The role of salt in fold-and-thrust belts,
Tectonophysics, 119, 67–88, 1985.
Davy, P. and Cobbold, P. R.: Experiments on shortening of a 4-layer model of
the continental lithosphere, Tectonophysics, 188, 1–25,
https://doi.org/10.1016/0040-1951(91)90311-F, 1991.
Dell'Ertole, D. and Schellart, W. P.: The development of sheath folds in
viscously stratified materials in simple shear conditions: An analogue
approach, J. Struct. Geol., 56, 129–141, https://doi.org/10.1016/j.jsg.2013.09.002,
2013.
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., McClay, K. R., Hempton, M., and Smit, D.: Salt tectonics above complex basement extensional fault systems: results from analogue modelling. Geological Society, London, Petroleum Geology Conference Series, 6, 1631–1648, https://doi.org/10.1144/0061631, 2005.
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.
Dooley, T. P., Jackson, M. P. A., and Hudec, M. R.: Inflation and deflation of deeply buried salt stocks during lateral shortening, J. Struct. Geol., 31, 582–600, https://doi.org/10.1016/j.jsg.2009.03.013, 2009.
Duffy, O. B., Dooley, T. P., Hudec, M. R., Jackson, M. P. A., Fernandez, N.,
Jackson, C. A. L., and Soto, J. I.: Structural evolution of salt-influenced
fold-and-thrust belts: a synthesis and new insights from basins containing
isolated salt diapirs, J. Struct. Geol., 114, 206–221, https://doi.org/10.1016/j.jsg.2018.06.024, 2018.
Duffy, O. B., Dooley, T. P., Hudec, M. R., Fernandez, N., Jackson, C. A. L., and Soto, J. I.: Principles of shortening in salt basins containing isolated minibasins, Basin Res., 33, 2089–2117, https://doi.org/10.1111/bre.12550, 2021.
Duffy, O., Hudec, M., Peel, F., Apps, G., Bump, A., Moscardelli, L., Dooley, T., Bhattacharya, S., Wisian, K., and Shuster, M.: The Role of Salt Tectonics in the Energy Transition: An Overview and Future Challenges, Tektonika, 1, 18–48, https://doi.org/10.55575/TEKTONIKA2023.1.1.11, 2023.
European Commission, Directorate-General for Research and Innovation: Europe’s 2030 climate and energy targets – Research & innovation actions, Publications Office, https://data.europa.eu/doi/10.2777/0948 (last access: 21 November 2022), 2021.
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.
Ferrer, O., Roca, E., and Vendeville, B. C.: The role of salt layers in the
hangingwall deformation of kinked-planar extensional faults: insights from
3D analogue models and comparison with the Parentis Basin, Tectonophysics,
636, 338–350, 2014.
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,
Geological Society, London, Special Publications, 439, 487–509,
https://doi.org/10.1144/SP439.8, 2016.
Ferrer, O., Carola, E., McClay, K., and Bufaliza, N.: Analog modeling of
domino-style extensional basement fault systems with pre-kinematic salt,
AAPG Bull., 107, 23–47, https://doi.org/10.1306/08072221188, 2022a.
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, 2022b.
Fillon, C., Huismans, R. S., and van der Beek, P. P.: Syntectonic
sedimentation effects on the growth of fold-and-thrust belts, Geology, 41,
83–86, https://doi.org/10.1130/G33531.1, 2013.
García-Senz, J.: Cuenca extensiva del cretácico inferior en los Pirineos centrales, formación y subsecuente inversión, PhD thesis, Universitat de Barcelona, 307 pp., 2002.
García-Senz, J., and Ramírez, I.: Mapa geológico de España
1:50.000 (2a serie), Instituto Geológico y Minero de
España, Madrid, Hoja 213, Pont de Suert, 1997.
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, Am. Assoc. Pet. Geol. Bull., 89, 495–506,
https://doi.org/10.1306/12010404018, 2005.
Gasanzade, F., Pfeiffer, W. T., Witte, F., Tuschy, I., and Bauer, S.:
Subsurface renewable energy storage capacity for hydrogen, methane and
compressed air – A performance assessment study from the North German
Basin, Renewable and Sustainable Energy Reviews, 149, 111422,
https://doi.org/10.1016/J.RSER.2021.111422, 2021.
Gawthorpe, R. L. and Hurst, J. M.: Transfer zones in extensional basins:
their structural style and influence on drainage development and
stratigraphy, Journal of the Geological Society, 150, 1137–1152,
https://doi.org/10.1144/gsjgs.150.6.1137, 1993.
Gibbs, A. D.: Structural evolution of extensional basin margins, J. Geol. Soc.
London, 141, 609–620, https://doi.org/10.1144/gsjgs.141.4.0609, 1984.
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.
Granado, P., Roca, E., Strauss, P., Pelz, K., and Muñoz, J. A.: Structural styles in fold-and-thrust belts involving early salt structures:
The Northern Calcareous Alps (Austria), Geology, 47, 51–54, https://doi.org/10.1130/G45281.1, 2019.
Granado, P., Ruh, J. B., Santolaria, P., Strauss, P., and Muñoz, J. A.:
Stretching and Contraction of Extensional Basins With Pre-Rift Salt: A
Numerical Modeling Approach, Front. Earth Sci. (Lausanne), 9,
https://doi.org/10.3389/feart.2021.648937, 2021.
Graveleau, F., Malavieille, J., and Dominguez, S.: Experimental modelling of orogenic wedges: A review, Tectonophysics, 538, 1–66, https://doi.org/10.1016/j.tecto.2012.01.027, 2012.
Hansen, T. H., Clausen, O. R., and Andresen, 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.
Hudec, M. R. and Jackson, M. P. A.: Terra infirma: Understanding salt tectonics, Earth-Sci. Rev., 82, 1–28, https://doi.org/10.1016/j.earscirev.2007.01.001, 2007.
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.
Kehle, R. O.: The Origin of Salt Structures, in: Evaporites and
Hydrocarbons, edited by: Schreiber, B. C., Columbia University Press, New
York Chichester, West Sussex, 345–404,
https://doi.org/10.7312/schr91060-008, 1988.
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.
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., Jenyon, M. K., and Petersen, K.: The effect of basement faulting
on diapirism, J. Petrol. Geol., 16, 285–312,
https://doi.org/10.1111/j.1747-5457.1993.tb00339.x, 1993.
Lacombe, O., Mazzoli, S., von Hagke, C., Rosenau, M., Fillon, C., and
Granado, P.: Style of deformation and tectono-sedimentary evolution of
fold-and-thrust belts and foreland basins: From nature to models,
Tectonophysics, 767, 228163, https://doi.org/10.1016/j.tecto.2019.228163, 2019.
Le Calvez, J. H. and Vendeville, B. C.: Experimental designs to model along-
strike fault interaction, Journal of the Virtual Explorer, 7, 2,
https://doi.org/10.3809/JVIRTEX.2002.00043, 2002.
Lescoutre, R., Tugend, J., Brune, S., Masini, E., and Manatschal, G.:
Thermal Evolution of Asymmetric Hyperextended Magma-Poor Rift Systems:
Results From Numerical Modeling and Pyrenean Field Observations,
Geochem. Geophy. Geosy., 20, 4567–4587,
https://doi.org/10.1029/2019GC008600, 2019.
Letouzey, J., Colleta, B., Vially, R., and Chermette, J. C.: Evolution of salt-related structures in compressional settings, AAPG Memoir., 65, 41–60, https://doi.org/10.1306/M65604C3, 1995.
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.
López-Mir, B., Muñoz, J. A., and García-Senz, J.: Extensional salt tectonics in the partially inverted Cotiella post-rift basin (south-central Pyrenees): structure and evolution, Int. J. Earth Sci. (Geol. Rundsch.), 104, 419–434, https://doi.org/10.1007/s00531-014-1091-9, 2015.
Manatschal, G., Chenin, P., Lescoutre, R., Miró, J., Cadenas, P.,
Saspiturry, N., Masini, E., Chevrot, S., Ford, M., Jolivet, L., Mouthereau,
F., Thinon, I., Issautier, B., and Calassou, S.: The role of inheritance in
forming rifts and rifted margins and building collisional orogens: a
Biscay-Pyrenean perspective, BSGF – Earth Sci. Bull., 192, 55,
https://doi.org/10.1051/bsgf/2021042, 2021.
Martín-Chivelet, J., López-Gómez, J., Aguado, R., Arias, C., Arribas, J., Arribas, M. E., Aurell, M., Bádenas, B., Benito, M. I., Bover-Arnal, T., Casas-Sainz, A., Castro, J. M., Coruña, F., de Gea, G. A., Fornós, J. J., Fregenal-Martínez, M., García-Senz, J., Garófano, D., Gelabert, B., Giménez, J., González-Acebrón, L., Guimerà, J., Liesa, C. L., Mas, R., Meléndez, N., Molina, J. M., Muñoz, J. A., Navarrete, R., Nebot, M., Nieto, L. M., Omodeo-Salé, S., Pedrera, A., Peropadre, C., Quijada, I. E., Quijano, M. L., Reolid, M., Robador, A., Rodríguez-López, J. P., Rodríguez-Perea, A,, Rosales, I., Ruiz-Ortiz, P. A., Sàbat, F., Salas, R., Soria, A. R., Suarez-Gonzalez, P., and Vilas, L.: The
Late Jurassic–Early Cretaceous Rifting, in: The Geology of Iberia A
Geodynamic Approach, edited by: Quesada, C. and Oliveira, J. T., Regional
Geological Reviews, Springer Nature, 169–249,
https://doi.org/10.1007/978-3-030-11295-0_5, 2019a.
Martín-Chivelet, J., Floquet, M., García-Senz, J., Callapez, P. M.,
López-Mir, B., Muñoz, J. A., Barroso-Barcenilla, F., Segura, M.,
Ferreira Soares, A., Morgado Dinis, P., Fonseca Marques, J., and Arbués,
P.: Late Cretaceous Post-Rift to Convergence, in: The Geology of Iberia A
Geodynamic Approach, edited by: Quesada, C. and Oliveira, J. T., Regional
Geological Reviews, Springer Nature, 285–376,
https://doi.org/10.1007/978-3-030-11295-0_7, 2019b.
Martin-Roberts, E., Scott, V., Flude, S., Johnson, G., Haszeldine, R. S.,
and Gilfillan, S.: Carbon capture and storage at the end of a lost decade,
One Earth, 4, 1569–1584, https://doi.org/10.1016/j.oneear.2021.10.002,
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.: The geometries and kinematics of inverted fault systems: A
review of analogue model 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.: Analogue Models of Contractional Thrust Wedges – The Dynamic
Effects of Syntectonic Sedimentation and Syntectonic Erosion, in: International Conference and Exhibition, Melbourne, Australia, 13–16 September 2015,
https://doi.org/10.1190/ice2015-2209023, 2015.
McClay, K. R., Dooley, T., 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.
Mencós, 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, 34, 1452–1474, https://doi.org/10.1002/2014TC003692, 2015.
Miocic, J. M., Alcalde, J., Heinemann, N., Marzan, I., and Hangx, S.: Toward
Energy-Independence and Net-Zero: The Inevitability of Subsurface Storage in
Europe, ACS Energy Lett., 7, 2486–2489,
https://doi.org/10.1021/acsenergylett.2c01303, 2022.
Miró, J., Manatschal, G., Cadenas, P., and Muñoz, J. A.:
Reactivation of a hyperextended rift system: The Basque–Cantabrian Pyrenees
case, Basin Res., 33, 3077–3101, https://doi.org/10.1111/bre.12595,
2021.
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.
Moragas, M., Vergés,
J., Nalpas, T., Saura, E., Martín-Martín, J. D., Messager, 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.
Moragas, M., Vergés, J., Saura, E., Martín-Martín, J. D.,
Messager, G., Merino-Tomé, Ó., Suárez-Ruiz, I., Razin, P.,
Grélaud, C., Malaval, M., Joussiaume, R., and Hunt, D. W.: Jurassic
rifting to post-rift subsidence analysis in the Central High Atlas and its
relation to salt diapirism, Basin Res., 30, 336–362,
https://doi.org/10.1111/bre.12223, 2018.
Morley, C. K., Nelson, R. A., Patton, T. L., and Munn, S. G.: Transfer Zones
in the East African Rift System and Their Relevance Hydrocarbon Eploration
Rifts, Am. Assoc. Petr. Geol. B., 74,
1234–1253, 1990.
Mugnier, J. L., Baby, P., Coletta, B., Vinour, P., Bale, P., and Leturmy, P.:
Thrust geometry controlled by erosion and sedimentation: A view from
analogue models, Geology, 25, 427–430, 1997.
Muñoz, J. A.: Evolution of a continental collision belt: ECORS-Pyrenees
crustal balanced cross-section, in: Thrust Tectonics, edited by: McClay, K. R.,
London, Chapman and Hall, 235–246, 1992.
Muñoz, J. A., Mencos, J., Roca, E., Carrera, N., Gratacós, O.,
Ferrer, O., and Fernández, O.: The structure of the
South-Central-Pyrenean fold and thrust belt as constrained by subsurface
data, Geol. Acta, 16, 439–460,
https://doi.org/10.1344/GeologicaActa2018.16.4.7, 2018.
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.
Peacock, D. C. P. and Sanderson, D. J.: Displacements, segment linkage and
relay ramps in normal fault zones, J. Struct. Geol., 13,
721–733, https://doi.org/10.1016/0191-8141(91)90033-F, 1991.
Pinheiro, L. M., Wilson, R. C. L., Pena dos Reis, R., Whitmarsh, R. B., and
Ribeiro, A.: The western Iberia Margin: a geophysical and geological
overview, in: Proceedings of the Ocean Drilling Program, Scientific Results,
vol. 149, edited by: Whitmarsh, R. B., Sawyer, D. S., Klaus, A., and Masson,
D. G., Ocean Drilling Program, 1–23,
https://doi.org/10.2973/odp.proc.sr.149.246.1996, 1996.
Pla, O., Roca, E., Xie, H., Izquierdo-Llavall, E., Muñoz, J. A., Rowan,
M. G., Ferrer, O., Gratacós, Ò., Yuan, N., and Huang, S.: Influence
of Syntectonic Sedimentation and Décollement Rheology on the Geometry
and Evolution of Orogenic Wedges: Analog Modeling of the Kuqa
Fold-and-Thrust Belt (NW China), Tectonics, 38, 2727–2755,
https://doi.org/10.1029/2018TC005386, 2019.
Puigdefàbregas, C., Muñoz, J. A., and Vergés, J.: Thrusting and
foreland basin evolution in the Southern Pyrenees, Thrust Tectonics,
247–254, https://doi.org/10.1007/978-94-011-3066-0_22, 1992.
Ramos, A., Lopez-Mir, B., Wilson, E. P., Granado, P., and Muñoz, J. A.: 3D
reconstruction of syn-tectonic strata in a salt-related orogen: learnings
from the Llert syncline (South-central Pyrenees), Geol. Acta, 18, 1–19, https://doi.org/10.1344/GeologicaActa2020.18.20,
2020.
Rasmussen, E. S., Lomholt, S., Andersen, C., and Vejbæk, O. V.: Aspects
of the structural evolution of the Lusitanian Basin in Portugal and the
shelf and slope area offshore Portugal, Tectonophysics, 300, 199–225,
https://doi.org/10.1016/S0040-1951(98)00241-8, 1998.
Ribeiro, A., Kullberg, M. C., Kullberg, J. C., Manuppella, G., and Phipps,
S.: A review of Alpine tectonics in Portugal: Foreland detachment in
basement and cover rocks, Tectonophysics, 184, 357–366,
https://doi.org/10.1016/0040-1951(90)90448-H, 1990.
Richardson, N. J., Underhill, J. R., and Lewis, G.: The role of evaporite
mobility in modifying subsidence patterns during normal fault growth and
linkage, Halten Terrace, Mid-Norway, Basin Res., 17, 203–223,
https://doi.org/10.1111/j.1365-2117.2005.00250.x, 2005.
Rime, V., Sommaruga, A., Schori, M., and Mosar, J.: Tectonics of the
Neuchâtel Jura Mountains: insights from mapping and forward modelling,
Swiss J. Geosci., 112, 563–578, https://doi.org/10.1007/S00015-019-00349-Y,
2019.
Robador, A. and Zamorano, M.: Mapa geológico de España 1:50.000
(2a serie), Hoja 212, Campo, Instituto Geológico y Minero
de España, Madrid, 1999.
Roma, M., Ferrer, O., Roca, E., Pla, O., Escosa, F. O., and Butillé, M.:
Formation and inversion of salt-detached ramp-syncline basins. Results from
analog modeling and application to the Columbrets Basin (Western
Mediterranean), Tectonophysics, 745, 214–228,
https://doi.org/10.1016/J.TECTO.2018.08.012, 2018a.
Roma, M., Vidal-Royo, O., McClay, K., Ferrer, O., and Muñoz, J. A.:
Tectonic inversion of salt-detached ramp-syncline basins as illustrated by
analog modeling and kinematic restoration, Interpretation, 6, T127–T144,
https://doi.org/10.1190/INT-2017-0073.1, 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, 2018c.
Rowan, M. G., and Vendeville, B. C.:
Foldbelts with early salt withdrawal and diapirism: Physical model and examples from the northern Gulf of Mexico and the Flinders Ranges, Australia, Mar. Petrol. Geol., 23, 871–891,
https://doi.org/10.1016/j.marpetgeo.2006.08.003, 2006.
Saïd, A., Baby, P., Chardon, D., and Ouali, J.: Structure,
paleogeographic inheritance, and deformation history of the Southern Atlas
foreland fold and thrust belt of Tunisia, Tectonics, 30, TC6004,
https://doi.org/10.1029/2011TC002862, 2011.
Sala, P., Pfiffner, O. A., and Frehner, M.: The Alpstein in three
dimensions: fold-and-thrust belt visualization in the Helvetic zone, eastern
Switzerland, Swiss J. Geosci., 107, 177–195, https://doi.org/10.1007/s00015-014-0168-6,
2014.
Santolaria, P., Granado, P., Carrera, N., Schneider, C. L., Ferrer, O.,
Snidero, M., Strauss, P., Pelz, K., Roca, E., and Muñoz, J. A.: From
downbuilding to contractional reactivation of salt-sediment systems:
Insights from analog modeling, Tectonophysics, 819, 229078,
https://doi.org/10.1016/j.tecto.2021.229078, 2021a.
Santolaria, P., Ferrer, O., Rowan, M. G., Snidero, M., Carrera, N., Granado,
P., Muñoz, J. A., Roca, E., Schneider, C. L., Piña, A., and Zamora,
G.: Influence of preexisting salt diapirs during thrust wedge evolution and
secondary welding: Insights from analog modeling, J. Struct. Geol., 149, 104374,
https://doi.org/10.1016/j.jsg.2021.104374, 2021b.
Santolaria, P., Granado, P., Wilson, E. P., de Matteis, M., Ferrer, O., M.,
Strauss, P., Pelz, K., König, M., Oteleanu, A. E., Roca, E., Muñoz,
J. A.: From salt-bearing rifted margins to fold-and-thrust belts. Insights
from analogue modelling and Northern Calcareous Alps case study, Tectonics, 41, e2022TC007503, https://doi.org/10.1029/2022TC007503,
2022.
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.
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.
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., 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., Elder Brady, J. A., Hoffmann-Rothe, A., Mengus, J. M.,
Montanari, D., and Nilforoushan, F.: Analogue benchmarks of shortening and
extension experiments, Geol. Soc. Spec. Publ., 253, 1–27,
https://doi.org/10.1144/GSL.SP.2006.253.01.01, 2006.
Séguret, M.: Étude tectonique des nappes et séries décollees de la partie centrale du versant sud des Pyrénées, Publications de l’Université de Sciences et Techniques de Languedoc, Montpellier, série Géologie Structurale, 2, 1–155, 1972.
Snidero, M., Muñoz, J.A., Carrera, N., Butillé, M., Mencos, J.,
Motamedi, H., Piryaei, A., Sàbat, F.: Temporal evolution of the Darmadan
salt diapir, eastern Fars region, Iran, Tectonophysics 766, 115–130,
https://doi.org/10.1016/j.tecto.2019.06.006.
Sommaruga, A.: Décollement tectonics in the Jura foreland
fold-and-thrust belt, Mar. Petrol. Geol., 16, 111–134, 1999.
Soto, J. I., Flinch, J., and Tari, G. (Eds.): Permo-Triassic Salt Provinces of Europe,
North Africa and the Atlantic Margins. Tectonics and Hydrocarbon Potential,
Elsevier, 608 pp., https://doi.org/10.1016/C2015-0-05796-3, 2017.
Stapel, G., Cloetingh, S., and Pronk, B.: Quantitative subsidence analysis
of the Mesozoic evolution of the Lusitanian basin (western Iberian margin),
Tectonophysics, 266, 493–507,
https://doi.org/10.1016/S0040-1951(96)00203-X, 1996.
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.: Detachment-controlled triangle zones in extension and inversion tectonics, Interpretation 2, SM29–SM38,
https://doi.org/10.1190/INT-2014-0026.1, 2014.
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.
Stewart, S. A., Harvey, M. J., Otto, S. C., and Weston, P. J.: Influence of
salt on fault geometry: Examples from the UK salt basins, Geol. Soc. Spec. Publ., 100, 175–202, https://doi.org/10.1144/GSL.SP.1996.100.01.12, 1996.
Stewart, S. A., Ruffell, A. H., and Harvey, M. J.: Relationship between
basement-linked and gravity-driven fault systems in the UKCS salt basins,
Mar. Petrol. Geol., 14, 581–604, https://doi.org/10.1016/S0264-8172(97)00008-1,
1997.
Storti, F. and McClay, K.R.: Influence of syntectonic sedimentation on
thrust wedges in analogue models, Geology, 23, 999–1002, 1995.
Strauss, P., Granado, P., and Muñoz, J. A.: Subsidence analysis of salt
tectonics-driven carbonate minibasins (Northern Calcareous Alps, Austria),
Basin Res., 33, 968–990, https://doi.org/10.1111/BRE.12500, 2021.
Tavani, S. and Granado, P.: Along-strike evolution of folding, stretching
and breaching of post-salt strata in the Plataforma Burgalesa extensional
forced fold system (northern Spain), Basin Res., 27,
573–585, https://doi.org/10.1111/bre.12089, 2015.
Tavani, S., Bertok, C., Granado, P., Piana, F., Salas, R., Vigna, B., and
Muñoz, J. A.: The Iberia-Eurasia plate boundary east of the Pyrenees,
Earth-Sci. Rev., 187, 314–337,
https://doi.org/10.1016/j.earscirev.2018.10.008, 2018.
Teixell, A.: The Ansó transect of the southern Pyrenees: Basement and
cover thrust geometries, J. Geol. Soc. London, 153, 301–310,
https://doi.org/10.1144/gsjgs.153.2.0301, 1996.
Tugend, J., Manatschal, G., Kusznir, N. J., Masini, E., Mohn, G., and
Thinon, I.: Formation and deformation of hyperextended rift systems:
Insights from rift domain mapping in the Bay of Biscay-Pyrenees, Tectonics,
33, 1239–1276, https://doi.org/10.1002/2014TC003529, 2014.
Velaj, T., Davison, I., Serjani, A., and Alsop, I.: Thrust tectonic and the role
of evaporites in the Ionian zone of the Albanides, AAPG Bull.,
83, 1408–1425, 1999.
Vendeville, B. C. and Jackson, M. P. A.:
The fall of diapirs during thin-skinned extension, Mar. Petrol. Geol.,
9, 354–371, https://doi.org/10.1016/0264-8172(92)90048-J, 1992.
Vendeville, B. C. and Nilsen, K. T.: Episodic growth of salt diapirs driven by horizontal shortening, in: Salt, Sediment, and Hydrocarbons, edited by: Travis, C. J., Harrison, H., Hudec, M. R., Vendeville, B. C., Peel, F. J., Perkins, B. F., SEPM Gulf Coast Section 16th Annual Research Foundation Conference, Houston, Texas, 285–295, 1995.
Vendeville, B. C., Hongxing Ge, and Jackson, M. P. A.: Scale models of salt
tectonics during basement-involved extension, Petrol. Geosci., 1,
179–183, https://doi.org/10.1144/petgeo.1.2.179, 1995.
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. Int., 43, 316–330,
https://doi.org/10.1016/0031-9201(86)90021-X, 1986.
White, N. J., Jackson, J. A., and McKenzie, D. P.: The relationship between
the geometry of normal faults and that of the sedimentary layers in their
hanging walls, J. Struct. Geol., 8, 897–909,
https://doi.org/10.1016/0191-8141(86)90035-0, 1986.
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.
Wilson, E. P.: Inversion of Transfer Zones – Model 01 Extension, TIB AV-Portal [video], https://doi.org/10.5446/60620, 2023a.
Wilson, E. P.: Inversion of Transfer Zones – Model 02 shortening, no surface processes, TIB AV-Portal [video], https://doi.org/10.5446/60621, 2023b.
Wilson, E. P.: Inversion of Transfer Zones - Model 03 shortening with syn-contractional sedimentation, TIB AV-Portal [video], https://doi.org/10.5446/60622, 2023c.
Withjack, M. O. and Callaway, S.: Active normal faulting beneath a salt
layer: An experimental study of deformation patterns in the cover sequence,
Am. Assoc. Pet. Geol. Bull., 84, 627–651,
https://doi.org/10.1306/c9ebce73-1735-11d7-8645000102c1865d, 2000.
Withjack, M. O., Olson, J., and Peterson, E.: Experimental Models of
Extensional Forced Folds, Am. Assoc. Pet. Geol. Bull., 74, 1038–1054,
https://doi.org/10.1306/0C9B23FD-1710-11D7-8645000102C1865D, 1990.
Yang, H., Yang, X., Zhang, H., Huang, X., Huang, W., and Zhang, N.: Active
fold deformation and crustal shortening rates of the Qilian Shan Foreland
Thrust Belt, NE Tibet, since the Late Pleistocene, Tectonophysics, 742–743,
84–100, https://doi.org/10.1016/J.TECTO.2018.05.019, 2018.
Ziegler, P. A. and van Hoorn, B.: Evolution of North Sea Rift System,
Extensional tectonics and stratigraphy of the North Atlantic margins, AAPG Memoir, 46,
471–500, https://doi.org/10.1306/M46497C31, 1989.
Zwaan, F. and Schreurs, G.: How oblique extension and structural inheritance
influence rift segment interaction: Insights from 4D analog models,
Interpretation, 5, SD119–SD138, https://doi.org/10.1190/int-2016-0063.1,
2017.
Zwaan, F., Schreurs, G., Buiter, S. J. H., Ferrer, O., Reitano, R., Rudolf, M., and Willingshofer, E.: Analogue modelling of basin inversion: a review and future perspectives, Solid Earth, 13, 1859–1905, https://doi.org/10.5194/se-13-1859-2022, 2022.
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 work focuses on the control of accommodation zones on extensional and subsequent inversion...
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