Articles | Volume 12, issue 8
https://doi.org/10.5194/se-12-1987-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-12-1987-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
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
Institute of Geophysics of the Czech Academy of Sciences, Boční II/1401, 14131 Prague, Czech Republic
Prokop Závada
Institute of Geophysics of the Czech Academy of Sciences, Boční II/1401, 14131 Prague, Czech Republic
Fabian Jähne-Klingberg
Federal Institute for Geosciences and Natural Resources, Stilleweg 2, 30655 Hanover, Germany
Piotr Krzywiec
Institute of Geological Sciences, Polish Academy of Sciences, Twarda 51/55, 00-818 Warsaw, Poland
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M. Warsitzka, J. Kley, and N. Kukowski
Solid Earth, 6, 9–31, https://doi.org/10.5194/se-6-9-2015, https://doi.org/10.5194/se-6-9-2015, 2015
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This paper summarizes the results of scaled analogue experiments examining the kinematics of salt flow and the formation of salt pillows due to basement faulting and subsequent sedimentation. Our experimental results reveal that salt above a basement normal fault can flow downward or upward depending on the direction of the pressure gradient within the salt layer. Due to upward flow driven by differential loading, salt pillows can form above the higher basement block.
Piotr Krzywiec, Mateusz Kufrasa, Paweł Poprawa, Stanisław Mazur, Małgorzata Koperska, and Piotr Ślemp
Solid Earth, 13, 639–658, https://doi.org/10.5194/se-13-639-2022, https://doi.org/10.5194/se-13-639-2022, 2022
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Legacy 2-D seismic data with newly acquired 3-D seismic data were used to construct a new model of geological evolution of NW Poland over last 400 Myr. It illustrates how the destruction of the Caledonian orogen in the Late Devonian–early Carboniferous led to half-graben formation, how they were inverted in the late Carboniferous, how the study area evolved during the formation of the Permo-Mesozoic Polish Basin and how supra-evaporitic structures were inverted in the Late Cretaceous–Paleogene.
Łukasz Słonka and Piotr Krzywiec
Solid Earth, 11, 1097–1119, https://doi.org/10.5194/se-11-1097-2020, https://doi.org/10.5194/se-11-1097-2020, 2020
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This paper shows the results of seismic interpretations that document the presence of large Upper Jurassic carbonate buildups in the Miechów Trough (S Poland). Our work fills the gap in recognition of the Upper Jurassic carbonate depositional system of southern Poland. The results also provide an excellent generic reference point, showing how and to what extent seismic data can be used for studies of carbonate depositional systems, in particular for the identification of the carbonate buildups.
M. Warsitzka, J. Kley, and N. Kukowski
Solid Earth, 6, 9–31, https://doi.org/10.5194/se-6-9-2015, https://doi.org/10.5194/se-6-9-2015, 2015
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This paper summarizes the results of scaled analogue experiments examining the kinematics of salt flow and the formation of salt pillows due to basement faulting and subsequent sedimentation. Our experimental results reveal that salt above a basement normal fault can flow downward or upward depending on the direction of the pressure gradient within the salt layer. Due to upward flow driven by differential loading, salt pillows can form above the higher basement block.
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)
Analogue modelling of basin inversion: a review and future perspectives
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
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
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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.
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
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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.
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
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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.
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
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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.
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
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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
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
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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.
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
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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.
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.
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
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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.
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
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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.
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
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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.
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
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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.
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
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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.
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
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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.
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
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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.
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
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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.
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
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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.
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
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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.
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
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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.
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
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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.
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
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Past strong earthquakes can produce topographic deformations, often
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
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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.
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
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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.
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
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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.
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
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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.
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
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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.
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
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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.
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
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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.
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
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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.
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
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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.
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
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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.
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
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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.
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
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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.
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
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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.
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
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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.
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
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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.
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
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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
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
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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.
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
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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.
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
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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.
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
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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.
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
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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.
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
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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.
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
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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.
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
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We propose a new exploration of the concept of
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
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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.
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
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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.
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
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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.
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
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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.
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. a, b, c
Adam, J., Ge, Z., and Sanchez, M.: Post-rift salt tectonic evolution and key
control factors of the Jequitinhonha deepwater fold belt, central Brazil
passive margin: Insights from scaled physical experiments, Mar. Pet. Geol.,
37, 70–100, https://doi.org/10.1016/j.marpetgeo.2012.06.008, 2012. a
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. a
Allen, J. and Beaumont, C.: Impact of inconsistent density scaling on physical
analogue models of continental margin scale salt tectonics, J. Geophys. Res.-Sol. Ea., 117, B08103, https://doi.org/10.1029/2012JB009227, 2012. a, b
Allen, M. R., Griffiths, P. A., Craig, J., Fitches, W. R., and Whittington,
R. J.: Halokinetic initiation of Mesozoic tectonics in the southern North
Sea: a regional model, Geol. Mag., 131, 559–561,
https://doi.org/10.1017/S0016756800012164, 1994. a, b
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. Pet. Geol., 19, 727–754,
https://doi.org/10.1016/S0264-8172(02)00036-3, 2002. a
Athy, L. F.: Density, porosity, and compaction of sedimentary rocks, AAPG
Bull., 14, 1–24, https://doi.org/10.1306/3D93289E-16B1-11D7-8645000102C1865D, 1930. a, b
Augustin, N., Devey, C. W., Van der Zwan, F. M., Feldens, P., Tominaga, M.,
Bantan, R. A., and Kwasnitschka, T.: The rifting to spreading transition in
the Red Sea, Earth Planet. Sc. Lett., 395, 217–230,
https://doi.org/10.1016/j.epsl.2014.03.047, 2014. a
Baldschuhn, R., Binot, F., Fleig, S., Kockel, F., (Hrsg.) unter Mitarbeit von:
Best, G., Brückner-Röhling, S., Deneke, E., Frisch, U., Hoffmann, N.,
Jürgens, U., Krull, P., Röhling, H.-G., Schmitz, J.,
Sattler-Kosinowski, S., Stancu-Kristoff, G., and Zirngast, M.:
Geotektonischer Atlas von Nordwest-Deutschland und dem deutschen
Nordsee-Sektor, Strukturen, Strukturentwicklung, Paläogeographie, Geol.
Jahrb., A, 153, 1–88, 3 CD–ROMs, 2001. a, b, c
Best, G.: Floßtektonik in Norddeutschland: Erste Ergebnisse
reflexionsseismischer Untersuchungen an der Salzstruktur “Oberes
Allertal”, Z. Dtsch. Geol. Ges., 147, 455–464, 1996. a
Bishop, D. J.: Regional distribution and geometry of salt diapirs and
supra-Zechstein Group faults in the western and central North Sea, Mar. Petrol. Geol., 13, 355–364, https://doi.org/10.1016/0264-8172(95)00081-X,
1996. a
Bishop, D. J., Buchanan, P. G., and Bishop, C. J.: Gravity-driven thin-skinned
extension above Zechstein Group evaporites in the western central North Sea:
an application of computer-aided section restoration techniques, Mar. Pet.
Geol., 12, 115–135, https://doi.org/10.1016/0264-8172(95)92834-J, 1995. a, b
Bodego, A. and Agirrezabala, L. M.: Syn-depositional thin-and thick-skinned
extensional tectonics in the mid-Cretaceous Lasarte sub-basin, western
Pyrenees, Basin Res., 25, 594–612,
https://doi.org/10.1111/bre.12017, 2013. a
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, 55–88,
https://doi.org/10.1016/j.tecto.2011.11.014, 2012. a, b
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. a
Brun, J.-P. and Mauduit, T. P.-O.: Salt rollers: structure and kinematics from
analogue modelling, Mar. Pet. Geol., 26, 249–258,
https://doi.org/10.1016/j.marpetgeo.2008.02.002, 2009. a
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. Lond., Spec. Pub., 363, 395–408, https://doi.org/10.1144/SP363.18, 2012. a
Byerlee, J.: Friction of rocks, Pure and applied geophysics, 116, 615–626,
https://doi.org/10.1007/978-3-0348-7182-2_4, 1978. a
Cámara, P.: Inverted turtle salt anticlines in the eastern
Basque-Cantabrian basin, Spain, Mar. Petrol. Geol., 117, 104358,
https://doi.org/10.1016/j.marpetgeo.2020.104358, 2020. a
Chapman, T. J.: The Permian to Cretaceous structural evolution of the Western
Approaches Basin (Melville sub-basin), UK, in: Inversion Tectonics,
Geological Society of London, 44, 177–200
https://doi.org/10.1144/GSL.SP.1989.044.01.11, 1989. a
Clausen, O. R. and Pedersen, P. K.: Late Triassic structural evolution of the
southern margin of the Ringkøbing-Fyn High, Denmark, Mar. Pet. Geol., 16,
653–665, https://doi.org/10.1016/S0264-8172(99)00026-4, 1999. a
Coleman, A. J., Jackson, C. A.-L., and Duffy, O. B.: Balancing sub-and
supra-salt strain in salt-influenced rifts: Implications for extension
estimates, J. Struct. Geol., 102, 208–225, https://doi.org/10.1016/j.jsg.2017.08.006,
2017. a
Dadlez, R., Narkiewicz, M., Stephenson, R. A., Visser, M. T. M., and Van Wees,
J. D.: Tectonic evolution of the Mid-Polish Trough: modelling implications
and significance for central European geology, Tectonophysics, 252,
179–195, https://doi.org/10.1016/0040-1951(95)00104-2, 1995. a
Dahlen, F. A.: Critical taper model of fold-and-thrust belts and accretionary
wedges, Annu. Rev. Earth Planet. Sci., 18, 55–99, https://doi.org/10.1146/annurev.ea.18.050190.000415, 1990. a, b
Dancer, P. N., Algar, S. T., and Wilson, I. R.: Structural evolution of the
Slyne Trough, in: Petroleum Geology of Northwest Europe: Proceedings of the
5th Conference, Geological Society, London,
5, 445–453, https://doi.org/10.1144/0050445, 1999. a
Dooley, T. P., 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. Lond., Spec. Pub., 212, 151–167,
https://doi.org/10.1144/GSL.SP.2003.212.01.10, 2003. a, b
Dooley, T. P., McClay, K. R., Hempton, M., and Smit, D.: Salt tectonics above
complex basement extensional fault systems: results from analogue modelling,
in: Geological Society, London, Petroleum Geology Conference series,
Geological Society of London, 6, 1631–1648, https://doi.org/10.1144/0061631, 2005. a, b, c, d, e
Dooley, T. P., Hudec, M. R., Carruthers, D., Jackson, M. P. A., and Luo, G.:
The effects of base-salt relief on salt flow and suprasalt deformation
patterns–Part 1: Flow across simple steps in the base of salt,
Interpretation, 5, 1–23, https://doi.org/10.1190/INT-2016-0087.1, 2017. a, b, c
Duffy, O. B., Gawthorpe, R. L., Docherty, M., and Brocklehurst, S. H.: Mobile
evaporite controls on the structural style and evolution of rift basins:
Danish Central Graben, North Sea, Basin Res., 25, 310–330,
https://doi.org/10.1111/bre.12000, 2013. a
England, P. and McKenzie, D.: A thin viscous sheet model for continental
deformation, Geophys. J. Int., 70, 295–321,
https://doi.org/10.1111/j.1365-246X.1982.tb04969.x, 1982. a
Fazlikhani, H., Fossen, H., Gawthorpe, R. L., Faleide, J. I., and Bell, R. E.:
Basement structure and its influence on the structural configuration of the
northern North Sea rift, Tectonics, 36, 1151–1177,
https://doi.org/10.1002/2017TC004514, 2017. a
Ferrer, O., Roca, E., Benjumea, B., Muñoz, J. A., Ellouz, N., and Marconi Team: The deep seismic reflection MARCONI-3 profile: Role of extensional
Mesozoic structure during the Pyrenean contractional deformation at the
eastern part of the Bay of Biscay, Mar. Petrol. Geol., 25,
714–730, https://doi.org/10.1016/j.marpetgeo.2008.06.002, 2008. a
Ferrer, O., Jackson, M. P. A., Roca, E., and Rubinat, M.: Evolution of salt
structures during extension and inversion of the Offshore Parentis Basin
(Eastern Bay of Biscay), Geol. Soc. Lond., Spec. Pub., 363, 361–380,
https://doi.org/10.1144/SP363.16, 2012. a
Ferrer, O., Roca, E., and Vendeville, B.: 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, https://doi.org/10.1016/j.tecto.2014.09.013, 2014. a, b
Ferrer, O., Gratacós, O., Roca, E., and Muñoz, J. A.: Modeling the
interaction between presalt seamounts and gravitational failure in
salt-bearing passive margins: The Messinian case in the northwestern
Mediterranean Basin, Interpretation, 5, 99–117,
https://doi.org/10.1190/INT-2016-0096.1, 2017. a, b
Fort, X., Brun, J.-P., and Chauvel, F.: Salt tectonics on the Angolan margin,
synsedimentary deformation processes, AAPG Bull., 88, 1523–1544,
https://doi.org/10.1306/06010403012, 2004. a, b, c, d
Gaullier, V., Brun, J. P., Gue, G., and Lecanu, H.: Raft tectonics: the
effects of residual topography below a salt décollement, Tectonophysics,
228, 363–381, https://doi.org/10.1016/0040-1951(93)90349-O, 1993. a
Ge, H., Jackson, M. P. A., and Vendeville, B. C.: Kinematics and dynamics of
salt tectonics driven by progradation, AAPG Bull., 81, 398–423,
https://doi.org/10.1306/522B4361-1727-11D7-8645000102C1865D, 1997. a, b, c
Ge, Z., Gawthorpe, R. L., Rotevatn, A., and Thomas, M. B.: Impact of normal
faulting and pre-rift salt tectonics on the structural style of
salt-influenced rifts: The Late Jurassic Norwegian Central Graben, North
Sea, Basin Res., 29, 674–698, https://doi.org/10.1111/bre.12219,
2017. a, b, c
Ge, Z., Rosenau, M., Warsitzka, M., and Gawthorpe, R. L.: Overprinting translational domains in passive margin salt basins: insights from analogue modelling, Solid Earth, 10, 1283–1300, https://doi.org/10.5194/se-10-1283-2019, 2019a. a, b
Geil, K.: The development of salt structures in Denmark and adjacent areas:
the role of basin floor dip and differential pressure, First Break, 9,
https://doi.org/10.3997/1365-2397.1991022, 1991. a, b, c
Geluk, M. C.: Stratigraphy and tectonics of Permo-Triassic basins in the
Netherlands and surrounding areas, PhD thesis, Utrecht University, 152 pp., 2005. a
Gemmer, L., Ings, S. J., Medvedev, S., and Beaumont, C.: Salt tectonics driven
by differential sediment loading: stability analysis and finite-element
experiments, Basin Res., 16, 199–218,
https://doi.org/10.1111/j.1365-2117.2004.00229.x, 2004. a
Gibbs, A. D.: Clyde Field growth fault secondary detachment above basement
faults in North Sea, AAPG Bull., 68, 1029–1039,
https://doi.org/10.1306/AD4616BF-16F7-11D7-8645000102C1865D, 1984. a
Griffiths, P. A., Allen, M. R., Craig, J., Fitches, W. R., and Whittington,
R. J.: Distinction between fault and salt control of Mesozoic sedimentation
on the southern margin of the Mid-North Sea High, Geol. Soc. Lond., Spec.
Pub., 91, 145–159, https://doi.org/10.1144/GSL.SP.1995.091.01.08, 1995. a, b
Heaton, R. C., Jackson, M. P. A., Bamahmoud, M., and Nani, A. S. O.:
Superposed Neogene extension, contraction, and salt canopy emplacement in
the Yemeni Red Sea, in: Salt tectonics: a global perspective, edited by:
Jackson, M. P. A., Roberts, D. G., and Snelson, S., 65, 333–351,
AAPG Mem., 1995. a
Høiland, O., Kristensen, J., and Monsen, T.: Mesozoic evolution of the
Jæren High area, Norwegian Central North Sea, in: Petroleum Geology of
Northwest Europe: Proceedings of the 4th Conference,
The Geological Society, London, Geological Society, London,
4, 1189–1195, https://doi.org/10.1144/0041189, 1993. a
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. a
Hudec, M. R., Jackson, M. P. A., and Schultz-Ela, D. D.: The Paradox of
Minibasin Subsidence into Salt, Geol. Soc. Am. Bull., 121,
201–221, https://doi.org/10.1130/B26275.1, 2009. a
Hughes, M. and Davison, I.: Geometry and growth kinematics of salt pillows in
the southern North Sea, Tectonophysics, 228, 239–254,
https://doi.org/10.1016/0040-1951(93)90343-I, 1993. a, b, c, d
Jackson, C. A.-L., Jackson, M. P. A., and Hudec, M. R.: Understanding the
kinematics of salt-bearing passive margins: A critical test of competing
hypotheses for the origin of the Albian Gap, Santos Basin, offshore Brazil,
GSA Bull., 127, 1730–1751, https://doi.org/10.1130/B31290.1, 2015. a
Jackson, C. A.-L., Elliott, G. M., Royce-Rogers, E., Gawthorpe, R. L., and Aas,
T. E.: Salt thickness and composition influence rift structural style,
northern North Sea, offshore Norway, Basin Res., 31, 514–538,
https://doi.org/10.1111/bre.12332, 2019. a
Jackson, M. P. A. and Cramez, C.: Seismic recognition of salt welds in salt
tectonics regimes, in: Gulf of Mexico salt tectonics, associated processes
and exploration potential: Gulf Coast Section SEPM Foundation, 10th Annual
Research Conference, SEPM Society for Sedimentary Geology,
66–71, https://doi.org/10.5724/gcs.89.10.0066, 1989. a
Jackson, M. P. A. and Talbot, C. J.: External shapes, strain rates, and
dynamics of salt structures, Geological Society of America Bulletin, 97,
305–323, https://doi.org/10.1130/0016-7606(1986)97<305:ESSRAD>2.0.CO;2, 1986. a
Jaeger, J. C., Cook, N. G. W., and Zimmerman, R.: Fundamentals of Rock
Mechanics, Blackwell Publishing, 4 Edn., 488 pp., 2007. a
Jammes, S., Manatschal, G., Lavier, L., and Masini, E.: Tectonosedimentary
evolution related to extreme crustal thinning ahead of a propagating ocean:
Example of the western Pyrenees, Tectonics, 28, TC4012, https://doi.org/10.1029/2008TC002406,
2009. a
Jammes, S., Manatschal, G., and Lavier, L.: Interaction between prerift salt
and detachment faulting in hyperextended rift systems: The example of the
Parentis and Mauléon basins (Bay of Biscay and western Pyrenees), AAPG
Bull., 94, 957–975, https://doi.org/10.1306/12090909116, 2010. a, b
Jensen, L. and Sørensen, K.: Tectonic framework and halokinesis of the
Nordkapp Basin, Barents Sea, in: Structural and Tectonic Modelling and its
Application to Petroleum Geology, edited by: Larsen, R. M., Brekke, H.,
Larsen, B. T., and Talleraas, E., Elsevier,
1, 109–120, https://doi.org/10.1016/B978-0-444-88607-1.50012-7, 1992. a
Jenyon, M. K.: Basin-edge diapirism and updip salt flow in Zechstein of
southern North Sea, AAPG Bull., 69, 53–64,
https://doi.org/10.1306/AD461B88-16F7-11D7-8645000102C1865D, 1985. a
Kockel, F. E., (mit Beiträgen von Baldschuhn, R., Best, G., Binot, F.,
Frisch, U., Gross, U., Jürgens, U., Röhling, H.-G., and
Sattler-Kosinowski, S.: Structural and Palaeogeographical Development of the
German North Sea Sector, Beitr. Reg. Geol. Erde, 26, 96 pp., 1995. a
Koyi, H., Talbot, C. J., and Tørudbakken, B. O.: Salt Tectonics in the
Northeastern Nordkapp Basin, Southwestern Barents Sea, in: Salt tectonics: a
global perspective, edited by: Jackson, M. P. A., Roberts, D. G., and Snelson,
S., AAPG Mem., 65, 437–447, 1995. a
Krézsek, C., Adam, J., and Grujic, D.: Mechanics of fault and expulsion
rollover systems developed on passive margins detached on salt: insights from
analogue modelling and optical strain monitoring, Geol. Soc. Lond., Spec.
Pub., 292, 103–121, https://doi.org/10.1144/SP292.6, 2007. a, b
Krzywiec, P.: Triassic-Jurassic evolution of the Pomeranian segment of the
Mid-Polish Trough – basement tectonics and subsidence patterns, Geol.
Quart., 50, 139–150, 2006a. a
Krzywiec, P.: Structural inversion of the Pomeranian and Kuiavian segments of
the Mid-Polish Trough – lateral variations in timing and structural style,
Geol. Quart., 50, 151–168, 2006b. a
Krzywiec, P.: Mesozoic and Cenozoic evolution of salt structures within the
Polish basin: An overview, Geol. Soc. Lond., Spec. Pub., 363, 381–394,
https://doi.org/10.1144/SP363.17, 2012. a, b
Krzywiec, P., Peryt, T. M., Kiersnowski, H., Pomianowski, P., Czapowski, G.,
and Kwolek, K.: Permo-Triassic Evaporites of the Polish Basin and Their
Bearing on the Tectonic Evolution and Hydrocarbon System, an Overview, in:
Permo-Triassic Salt Provinces of Europe, North Africa and the Atlantic
Margins, edited by: Soto, J. I., Flinch, J. F., and Tari, G.,
Elsevier, Amsterdam, Netherlands, 1 Edn., 243–261,
https://doi.org/10.1016/B978-0-12-809417-4.00012-4, 2017. a
Kusznir, N. J., Stovba, S. M., Stephenson, R. A., and Poplavskii, K. N.: The
formation of the northwestern Dniepr-Donets Basin: 2-D forward and reverse
syn-rift and post-rift modelling, Tectonophysics, 268, 237–255,
https://doi.org/10.1016/S0040-1951(96)00230-2, 1996. a
Labaume, P. and Teixell, A.: Evolution of salt structures of the Pyrenean rift
(Chaînons Béarnais, France): From hyper-extension to tectonic inversion,
Tectonophysics, 228451, https://doi.org/10.1016/j.tecto.2020.228451, 2020. a, b, c, d
Lagabrielle, Y., Labaume, P., and de Saint Blanquat, M.: Mantle exhumation,
crustal denudation, and gravity tectonics during Cretaceous rifting in the
Pyrenean realm (SW Europe): Insights from the geological setting of the
lherzolite bodies, Tectonics, 29, TC4012, https://doi.org/10.1029/2009TC002588, 2010. a
Lagabrielle, Y., Asti, R., Duretz, T., Clerc, C., Fourcade, S., Teixell, A.,
Labaume, P., Corre, B., and Saspiturry, N.: A review of cretaceous
smooth-slopes extensional basins along the Iberia-Eurasia plate boundary: How
pre-rift salt controls the modes of continental rifting and mantle
exhumation, Earth-Sci. Rev., 201, 103071,
https://doi.org/10.1016/j.earscirev.2019.103071, 2020. a
LaVision, A.: StrainMaster Manual for DaVis 10.0., LaVision GmbH, Goettingen,
2018. a
Lewis, M. M., Jackson, C. A.-L., and Gawthorpe, R. L.: Salt-influenced normal
fault growth and forced folding: The Stavanger Fault System, North Sea,
J. Struct. Geol., 54, 156–173, https://doi.org/10.1016/j.jsg.2013.07.015,
2013. a
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. a
Loncke, L., Vendeville, B. C., Gaullier, V., and Mascle, J.: Respective
contributions of tectonic and gravity-driven processes on the structural
pattern in the Eastern Nile deep-sea fan: insights from physical
experiments, Basin Res., 22, 765–782,
https://doi.org/10.1111/j.1365-2117.2009.00436.x, 2010. a
Lopez-Mir, B., Muñoz, J. A., and Senz, J. G.: Restoration of basins driven
by extension and salt tectonics: Example from the Cotiella Basin in the
central Pyrenees, J. Struct. Geol., 69, 147–162,
https://doi.org/10.1016/j.jsg.2014.09.022, 2014. a, b
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., 104, 419–434, https://doi.org/10.1007/s00531-014-1091-9, 2015. a, b, c
Lymer, G., Vendeville, B. C., Gaullier, V., Chanier, F., and Gaillard, M.:
Using salt tectonic structures as proxies to reveal post-rift crustal
tectonics: The example of the Eastern Sardinian margin (Western Tyrrhenian
Sea), Mar. Petrol. Geol., 214–231,
https://doi.org/10.1016/j.marpetgeo.2018.05.037, 2018. a, b
Martín-Martín, J., Vergés, J., Saura, E., Moragas, M., Messager,
G., Baqués, V., Razin, P., Grélaud, C., Malaval, M., Joussiaume, R.,
et al.: Diapiric growth within an Early Jurassic rift basin: The Tazoult
salt wall (central High Atlas, Morocco), Tectonics, 36, 2–32,
https://doi.org/10.1002/2016TC004300, 2017. a
Maystrenko, Y. P., Bayer, U., and Scheck-Wenderoth, M.: Structure and
evolution of the Glueckstadt Graben due to salt movements, Int. J. Earth
Sci., 94, 799–814, https://doi.org/10.1007/s00531-005-0003-4, 2005. a, b
Maystrenko, Y. P., Bayer, U., and Scheck-Wenderoth, M.: Structure and
Evolution of the Glueckstadt Graben in Relation to the Other PostPermian
Subbasins of the Central European Basin System, in: Permo-Triassic Salt
Provinces of Europe, North Africa and the Atlantic Margins, edited by: Soto,
J. I., Flinch, J. F., and Tari, G., Elsevier, Amsterdam,
Netherlands, 1 Edn., 203–220, https://doi.org/10.1016/B978-0-12-809417-4.00010-0, 2017. a
McClay, K., Dooley, T., and Zamora, G.: Analogue models of delta systems above
ductile substrates, Geological Society, London, Special Publications, 216,
411–428, https://doi.org/10.1144/GSL.SP.2003.216.01.27, 2003. a
McClay, K., Munõz, J.-A., and García-Senz, J.: Extensional salt tectonics
in a contractional orogen: A newly identified tectonic event in the Spanish
Pyrenees, Geology, 32, 737–740, https://doi.org/10.1130/G20565.1, 2004. a
Mianaekere, V. and Adam, J.: “Halo-kinematic” sequence-stratigraphic
analysis of minibasins in the deepwater contractional province of the
Liguro-Provençal basin, Western Mediterranean, Mar. Petrol.
Geol., 104307, https://doi.org/10.1016/j.marpetgeo.2020.104307,
2020. a
Mitchell, D. J. W., Allen, R. B., Salama, W., and Abouzakm, A.:
Tectonostratigraphic framework and hydrocarbon potential of the Red Sea,
J. Petrol. Geol., 15, 187–210,
https://doi.org/10.1111/j.1747-5457.1992.tb00962.x, 1992. a
Mohr, M., Kukla, P. A., Urai, J., and Bresser, G.: Multiphase salt tectonic
evolution in NW Germany: seismic interpretation and retro-deformation, Int.
J. Earth Sci., 94, 917–940, https://doi.org/10.1007/s00531-005-0039-5, 2005. a, b
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. a, b, c
Mukherjee, S., Talbot, C. J., and Koyi, H. A.: Viscosity estimates of salt in
the Hormuz and Namakdan salt diapirs, Persian Gulf, Geol. Mag.,
147, 497–507, https://doi.org/10.1017/S001675680999077X, 2010. a
Nalpas, T. and Brun, J.-P.: Salt flow and diapirism related to extension at
crustal scale, Tectonophysics, 228, 349–362,
https://doi.org/10.1016/0040-1951(93)90348-N, 1993. a, b, c
Nilsen, K. T., Johansen, J. T., and Vendeville, B. C.: Influence of regional
tectonics on halokinesis in the Nordkapp Basin, Barents Sea, in: Salt
tectonics: a global perspective, edited by: Jackson, M. P. A., Roberts, D. G.,
and Snelson, S., AAPG Mem., 65, 413–436, 1996. a
O’Sullivan, C. M., Childs, C. J., Saqab, M. M., Walsh, J. J., and Shannon,
P. M.: The influence of multiple salt layers on rift-basin development; The
Slyne and Erris basins, offshore NW Ireland, Basin Res., 33, 2018–2048,
https://doi.org/10.1111/bre.12546, 2021. a
Panien, M., Schreurs, G., and Pfiffner, 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, 2006. a
Pascoe, R., Hooper, R., Storhaug, K., and Harper, H.: Evolution of extensional
styles at the southern termination of the Nordland Ridge, Mid-Norway: a
response to variations in coupling above Triassic salt, in: Geological
Society, London, Petroleum Geology Conference Series,
Geological Society of London, London, 5, 83–90, https://doi.org/10.1144/0050083, 1999. a
Peel, F. J.: The engines of gravity-driven movement on passive margins:
Quantifying the relative contribution of spreading vs. gravity sliding
mechanisms, Tectonophysics, 633, 126–142,
https://doi.org/10.1016/j.tecto.2014.06.023, 2014. a
Pena dos Reis, R., Pimentel, N., Fainstein, R., Reis, M., and Rasmussen, B.:
Influence of Salt Diapirism on the Basin Architecture and Hydrocarbon
Prospects of the Western Iberian Margin, in: Permo-Triassic Salt Provinces
of Europe, North Africa and the Atlantic Margins, edited by: Soto, J. I.,
Flinch, J. F., and Tari, G., Elsevier,
313–329, https://doi.org/10.1016/B978-0-12-809417-4.00015-X, 2017. a
Penge, J., Munns, J. W., Taylor, B., and Windle, T. M. F.: Rift–raft
tectonics: examples of gravitational tectonics from the Zechstein basins of
northwest Europe, in: Geological Society, London, Petroleum Geology
Conference series, edited by Fleet, A. J. and Boldy, S. A. R., Geological Society, London, 5,
201–213, 1999. a, b, c, d, e, f, g, h
Petersen, K., Clausen, O. R., and Korstgård, J. A.: Evolution of a
salt-related listric growth fault near the D-1 well, block 5605, Danish North
Sea: displacement history and salt kinematics, J. Struct. Geol., 14, 565–577, https://doi.org/10.1016/0191-8141(92)90157-R, 1992. a
Pichel, L. M., Jackson, C. A.-L., Peel, F., and Dooley, T. P.: Base-salt
relief controls salt-tectonic structural style, São Paulo Plateau, Santos
Basin, Brazil, Basin Res., 32, 453–484, https://doi.org/10.1111/bre.12375, 2020. a
Quirk, D. G., Schødt, N., Lassen, B., Ings, S. J., Hsu, D., Hirsch, K. K.,
and Von Nicolai, C.: Salt tectonics on passive margins: examples from
Santos, Campos and Kwanza basins, Geological Society, London, Special
Publications, 363, 207–244, https://doi.org/10.1144/SP363.10, 2012. a, b
Radies, D., Stollhofen, H., Hollmann, G., and Kukla, P.: Synsedimentary faults
and amalgamated unconformities: insights from 3D-seismic and core analysis of
the Lower Triassic Middle Buntsandstein, Ems Trough, north-western Germany,
Int. J. Earth Sci., 94, 863–875, https://doi.org/10.1007/s00531-005-0009-y, 2005. a
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. a
Rojo, L. A., Cardozo, N., Escalona, A., and Koyi, H.: Structural style and
evolution of the Nordkapp Basin, Norwegian Barents Sea, AAPG Bulletin, 103,
2177–2217, https://doi.org/10.1306/01301918028, 2019. a
Rojo, L. A., Koyi, H., Cardozo, N., and Escalona, A.: Salt tectonics in
salt-bearing rift basins: Progradational loading vs extension, J. Struct. Geol., 141, 104193,
https://doi.org/10.1016/j.jsg.2020.104193, 2020. a
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, 127–144,
https://doi.org/10.1190/INT-2017-0073.1, 2018. a, b, c
Rowan, M. G. and Lindsø, S.: Salt tectonics of the Norwegian Barents Sea
and northeast Greenland shelf, in: Permo-Triassic Salt Provinces of Europe,
North Africa and the Atlantic Margins, edited by: Soto, J. I., Flinch, J. F.,
and Tari, G., Elsevier, 265–286,
https://doi.org/10.1016/B978-0-12-809417-4.00013-6, 2017. a
Rowan, M. G., Peel, F. J., Vendeville, B. C., and Gaullier, V.: Salt tectonics
at passive margins: Geology versus models – Discussion, Mar. Pet. Geol.,
37, 184–194, https://doi.org/10.1016/j.marpetgeo.2012.04.007, 2012. a
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. a, b, c
Saspiturry, N., Razin, P., Baudin, T., Serrano, O., Issautier, B., Lasseur, E.,
Allanic, C., Thinon, I., and Leleu, S.: Symmetry vs. asymmetry of a
hyper-thinned rift: example of the Mauléon Basin (Western Pyrenees,
France), Mar. Petrol. Geol., 104, 86–105,
https://doi.org/10.1016/j.marpetgeo.2019.03.031, 2019. a
Saura, E., Ardèvol i Oró, L., Teixell, A., and Vergés, J.: Rising
and falling diapirs, shifting depocenters, and flap overturning in the
Cretaceous Sopeira and Sant Gervàs subbasins (Ribagorça Basin,
southern Pyrenees), Tectonics, 35, 638–662, https://doi.org/10.1002/2015TC004001,
2016. a, b, c
Schléder, Z., Urai, J. L., Nollet, S., and Hilgers, C.:
Solution-precipitation creep and fluid flow in halite: a case study of
Zechstein (Z1) rocksalt from Neuhof salt mine (Germany), Int. J. Earth
Sci., 97, 1045–1056, https://doi.org/10.1007/s00531-007-0275-y, 2008. a
Schultz-Ela, D. D.: Excursus on gravity gliding and gravity spreading, J.
Struct. Geol., 23, 725–731, https://doi.org/10.1016/S0191-8141(01)00004-9, 2001. a, b
Seni, S. J. and Jackson, M. P. A.: Sedimentary Record of Cretaceous and
Tertiary Salt Movement, East Texas Basin: Times, Rates, and Volumes of Salt
Flow and Their Implications for Nuclear Waste Isolation and Petroleum
Exploration, in: The University of Texas at Austin Bureau of Economic
Geology Report of Invesitgations, Bureau of Economic
Geology, 139, 89 pp., University of Texas of Austin, 1984. a
Sornette, A., Davy, P., and Sornette, D.: Fault growth in brittle-ductile
experiments and the mechanics of continental collisions, J. Geophys. Res.-Sol. Ea., 98, 12111–12139,
https://doi.org/10.1029/92JB01740, 1993. a
Stewart, S. A.: Detachment-controlled triangle zones in extension and
inversion tectonics, Interpretation, 2, 29–38,
https://doi.org/10.1190/INT-2014-0026.1, 2014. a, b
Stewart, S. A. and Clark, J. A.: Impact of salt on the structure of the
Central North Sea hydrocarbon fairways, Geological Society, London,
Petrol. Geol. Conf. Ser., 5, 179–200, https://doi.org/10.1144/0050179,
1999. a, b, c, d
Stewart, S. A. and Coward, M. P.: Genetic interpretation and mapping of salt
structures, First Break, 14, 135–141, https://doi.org/10.3997/1365-2397.1996009,
1996. a
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. Lond.,
Spec. Pub., 100, 175–202, https://doi.org/10.1144/GSL.SP.1996.100.01.12, 1996. a, b, c
Stovba, S. M. and Stephenson, R. A.: Style and timing of salt tectonics in the
Dniepr-Donets Basin (Ukraine): implications for triggering and driving
mechanisms of salt movement in sedimentary basins, Mar. Pet. Geol., 19,
1169–1189, https://doi.org/10.1016/S0264-8172(03)00023-0, 2003. a
Stovba, S. M., Stephenson, R. A., and Kivshik, M.: Structural features and
evolution of the Dniepr-Donets Basin, Ukraine, from regional seismic
reflection profiles, Tectonophysics, 268, 127–147,
https://doi.org/10.1016/S0040-1951(96)00222-3, 1996. a
Strozyk, F., Urai, J. L., van Gent, H., de Keijzer, M., and Kukla, P. A.:
Regional variations in the structure of the Permian Zechstein 3 intrasalt
stringer in the northern Netherlands: 3D seismic interpretation and
implications for salt tectonic evolution, Interpretation, 2, 101–117,
https://doi.org/10.1190/INT-2014-0037.1, 2014. a
Strozyk, F., Reuning, L., Scheck-Wenderoth, M., and Tanner, D. C.: The
tectonic history of the Zechstein Basin in the Netherlands and Germany, in:
Permo-Triassic Salt Provinces of Europe, North Africa and the Atlantic
Margins, edited by: Soto, J. I., Flinch, J. F., and Tari, G., 221–241,
Elsevier, Amsterdam, Netherlands, 1 Edn.,
https://doi.org/10.1016/B978-0-12-809417-4.00011-2, 2017. a
Tanveer, M. and Korstgård, J. A.: Structural evolution of the Feda Graben
area–A new model, Mar. Pet. Geol., 26, 990–999,
https://doi.org/10.1016/j.marpetgeo.2008.04.010, 2009. a
Teixell, A., Labaume, P., and Lagabrielle, Y.: The crustal evolution of the
west-central Pyrenees revisited: inferences from a new kinematic scenario,
Comptes Rendus Geosci., 348, 257–267, https://doi.org/10.1016/j.crte.2015.10.010,
2016. a
Thomas, D. W. and Coward, M. P.: Mesozoic regional tectonics and South Viking
Graben formation: evidence for localized thin-skinned detachments during rift
development and inversion, Mar. Petrol. Geol., 13, 149–177,
https://doi.org/10.1016/0264-8172(95)00034-8, 1996. a, b, c
Troudi, H., Tari, G., Alouani, W., and Cantarella, G.: Styles of salt
tectonics in Central Tunisia: an overview, in: Permo-Triassic Salt
Provinces of Europe, North Africa and the Atlantic Margins, edited by: Soto,
J. I., Flinch, J. F., and Tari, G., Elsevier,
543–561, https://doi.org/10.1016/B978-0-12-809417-4.00026-4, 2017. a
Turcotte, D. L. and Schubert, G.: Geodynamics, Cambridge University Press,
third edn., 2014. a
Tvedt, A. B. M., Rotevatn, A., Jackson, C. A.-L., Fossen, H., and Gawthorpe,
R. L.: Growth of normal faults in multilayer sequences: a 3D seismic case
study from the Egersund Basin, Norwegian North Sea, J. Struct. Geol., 55,
1–20, https://doi.org/10.1016/j.jsg.2013.08.002, 2013. a, b, c
Tvedt, A. B. M., Rotevatn, A., and Jackson, C. A. L.: Supra-salt normal fault
growth during the rise and fall of a diapir: Perspectives from 3D seismic
reflection data, Norwegian North Sea, J. Struct. Geol., 91,
1–26, https://doi.org/10.1016/j.jsg.2016.08.001, 2016. a
Urai, J. L., Schléder, Z., Spiers, C. J., and Kukla, P. A.: Flow and
Transport Properties of Salt Rocks, in: Dynamics of Complex
Intracontinental Basins: The Central European Basin System, edited by:
Littke, R., Bayer, U., Gajewski, D., and Nelskamp, S.,
Springer-Verlag, Berlin, Heidelberg, 277–290, 2008. a, b, c, d
Vackiner, A. A., Antrett, P., Strozyk, F., Back, S., Kukla, P., and Stollhofen,
H.: Salt kinematics and regional tectonics across a Permian gas field: a
case study from East Frisia, NW Germany, Int. J. Earth Sci., 102,
1701–1716, https://doi.org/10.1007/s00531-013-0887-3, 2013. a, b
Van Gent, H., Urai, J. L., and De Keijzer, M.: The internal geometry of salt
structures – A first look using 3D seismic data from the Zechstein of the
Netherlands, J. Struct. Geol., 33, 292–311,
https://doi.org/10.1016/j.jsg.2010.07.005, 2011. a
Van Keken, P. E., Spiers, C. J., Van den Berg, A. P., and Muyzert, E. J.: The
effective viscosity of rocksalt: implementation of steady-state creep laws in
numerical models of salt diapirism, Tectonophysics, 225, 457–476,
https://doi.org/10.1016/0040-1951(93)90310-G, 1993. a, b, c
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, in: Mesozoic Resource Potential in the Southern
Permian Basin, edited by: Kilhams, B., Kukla, P. A., Mazur, S., McKie, T.,
Mijnlieff, H. F., and Van Ojik, K., Geol. Soc. (Lond.)
Spec. Publ., 469, 99–117, https://doi.org/10.1144/SP469.9, 2018. a
Vejbæk, O. V.: The Horn Graben, and its relationship to the Oslo Graben
and the Danish Basin, Tectonophysics, 178, 29–49,
https://doi.org/10.1016/0040-1951(90)90458-K, 1990. a, b
Vendeville, B. C.: Salt tectonics driven by sediment progradation: Part I –
Mechanics and kinematics, AAPG Bull., 89, 1071–1079,
https://doi.org/10.1306/03310503063, 2005. a, b
Vendeville, B. C. and Jackson, M. P. A.: The rise of diapirs during
thin-skinned extension, Mar. Pet. Geol., 9, 331–354,
https://doi.org/10.1016/0264-8172(92)90047-I, 1992. a
Vendeville, B. C., Ge, H., and Jackson, M. P. A.: Scale models of salt
tectonics during basement-involved extension, Petroleum Geoscience, 1,
179–183, https://doi.org/10.1144/petgeo.1.2.179, 1995. a, b, c
Vergés, J., Moragas, M., Martín-Martín, J. D., Saura, E.,
Casciello, E., Razin, P., Grélaud, C., Malaval, M., Joussiame, R.,
Messager, G., et al.: Salt tectonics in the Atlas mountains of Morocco, in:
Permo-Triassic Salt Provinces of Europe, North Africa and the Atlantic
Margins, edited by Soto, J. I., Flinch, J. F., and Tari, G., 563–579,
Elsevier, https://doi.org/10.1016/B978-0-12-809417-4.00027-6, 2017. a
Wagner, R., Leszczyński, K., Pokorski, J., and Gumulak, K.: Palaeotectonic
cross-sections through the Mid-Polish Trough, Geol. Quart., 46,
293–306, 2002. a
Walker, I. M. and Cooper, W. G.: The structural and stratigraphic evolution of
the northeast margin of the Sole Pit Basin, in: Proceedings of the 3rd
Conference on Petroleum geology of North West Europe, edited by: Brooks, J.
and Glennie, K. W., Graham & Trotman, London, 1, 263–275, 1987. a
Warsitzka, M., Kley, J., and Kukowski, N.: Analogue experiments of salt flow and pillow growth due to basement faulting and differential loading, Solid Earth, 6, 9–31, https://doi.org/10.5194/se-6-9-2015, 2015. a, b
Warsitzka, M., Kley, J., Jähne-Klingberg, F., and Kukowski, N.: Dynamics
of prolonged salt movement in the Glückstadt Graben (NW Germany) driven
by tectonic and sedimentary processes, Int. J. Earth Sci., 106, 131–155,
https://doi.org/10.1007/s00531-016-1306-3, 2017.
a, b
Warsitzka, M., Kukowski, N., and Kley, J.: Salt flow direction and velocity
during subsalt normal faulting and syn-kinematic sedimentation –
implications from analytical calculations, Geophys. J. Int., 213, 115–134, https://doi.org/10.1093/gji/ggx552, 2018. a, b
Warsitzka, M., Závada, P., Jähne-Klingberg, F., and Krzywiec, P.:
Analog laboratory experiments of gravity gliding in salt-bearing rift
basins [data set], https://doi.org/10.1594/PANGAEA.931848, 2021a. a
Warsitzka, M., Závada, P., Krýza, O., Pohlenz, A., and Rosenau, M.:
Ring-shear test data of quartz sand – silicate cenospheres mixtures used
for analogue experiments at the Institute of Geophysics of the Czech Academy
of Science, Prague, https://doi.org/10.5880/fidgeo.2021.024, 2021b. a
Watts, A. B., Karner, G., and Steckler, M. S.: Lithospheric flexure and the
evolution of sedimentary basins, Philos T. R. Soc. S.-A., 305,
249–281, https://doi.org/10.1098/rsta.1982.0036, 1982. a
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. a, b, c, d, e
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. a, b
Wong, T. E., Batjes, D. A. J., de Jager, J., and van Wetenschappen, K. N. A.:
Geology of the Netherlands, Amsterdam: Royal Netherlands Academy of Arts
and Sciences, 354 pp., 2007. a
Zoback, M. L. and Mooney, W. D.: Lithospheric buoyancy and continental
intraplate stresses, Int. Geol. Rev., 45, 95–118,
https://doi.org/10.2747/0020-6814.45.2.95, 2003. a
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, Global Planet. Change, 171, 110–133, https://doi.org/10.1016/j.gloplacha.2017.11.002, 2018. a
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. a, b
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.
A new analogue modelling approach was used to simulate the influence of tectonic extension and...