Articles | Volume 11, issue 4
https://doi.org/10.5194/se-11-1313-2020
© Author(s) 2020. 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-11-1313-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Short communication
| 
21 Jul 2020
Short communication |
| 21 Jul 2020
A reconstruction of Iberia accounting for Western Tethys–North Atlantic kinematics since the late-Permian–Triassic
Geosciences Environnement Toulouse (GET), Université de Toulouse, UPS, Univ. Paul Sabatier, CNRS, IRD, 14 av. Edouard Belin, 31400 Toulouse, France
Frédéric Mouthereau
Geosciences Environnement Toulouse (GET), Université de Toulouse, UPS, Univ. Paul Sabatier, CNRS, IRD, 14 av. Edouard Belin, 31400 Toulouse, France
Emmanuel Masini
M&U sas, 38120 Saint-Égrève, France
ISTerre, Université Grenoble Alpes, 38000 Grenoble, France
Riccardo Asti
Université de Rennes, CNRS, Géosciences Rennes‐UMR 6118, 35000 Rennes, France
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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.
Marine Larrey, Frederic Mouthereau, Damien Do Couto, Emmanuel Masini, Anthony Jourdon, Syvlain Calassou, and Veronique Miegebielle
EGUsphere, https://doi.org/10.5194/egusphere-2022-1166, https://doi.org/10.5194/egusphere-2022-1166, 2022
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Extension leading to the formation of ocean-continental transition can be highly oblique to the main direction of crustal thinning. Here we explore the case of a continental margin exposed in the Betics, north of the Alboran margin, that developed in back-arc setting perpendicular to the direction of retreating Gibraltar subduction. We show that transtension is the main mode of crustal deformation that best explains the formation of metamorphic domes, extensional basins and brittle faults.
Arnaud Vacherat, Stéphane Bonnet, and Frédéric Mouthereau
Earth Surf. Dynam., 6, 369–387, https://doi.org/10.5194/esurf-6-369-2018, https://doi.org/10.5194/esurf-6-369-2018, 2018
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The Ebro and Duero basins share a very common geological history. However, since the late Miocene, the Ebro basin has recorded important unfilling and excavation, whereas the Duero basin has only recorded limited incision and is considered to be still almost endorheic. Such a morphologic contrast led to important drainage reorganization and divide migration toward the Duero basin. Drainage area loss results in the lowering of the incision capacity of the Duero River, increasing this contrast.
Margaux Mouchené, Peter van der Beek, Sébastien Carretier, and Frédéric Mouthereau
Earth Surf. Dynam., 5, 125–143, https://doi.org/10.5194/esurf-5-125-2017, https://doi.org/10.5194/esurf-5-125-2017, 2017
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The Lannemezan megafan (northern Pyrenean foreland) was abandoned during the Quaternary and subsequently incised. We use numerical models to explore possible scenarios for the evolution of this megafan. We show that autogenic processes are sufficient to explain its evolution. Climate may have played a second-order role; in contrast base-level change, tectonic activity and flexural isostatic rebound do not appear to have influenced its evolution.
C. Clerc, A. Lahfid, P. Monié, Y. Lagabrielle, C. Chopin, M. Poujol, P. Boulvais, J.-C. Ringenbach, E. Masini, and M. de St Blanquat
Solid Earth, 6, 643–668, https://doi.org/10.5194/se-6-643-2015, https://doi.org/10.5194/se-6-643-2015, 2015
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The northern flank of the Pyrenean belt is an example of an inverted hot passive margin. We provide a data set of more than 100 peak-temperature estimates by RSCM and 18 new radiogenic ages from metamorphic and magmatic rocks from the North Pyrenean Zone. The results indicate a first-order control of the thermal gradient by the intensity of the Cretaceous crustal thinning. The highest grades of metamorphism are associated with the areas where mantle peridotites have been unroofed or exhumed.
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
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
Construction of the Ukrainian Carpathian Wedge from low-temperature thermochronology and tectono-stratigraphic analysis
Late Cretaceous–early Palaeogene inversion-related tectonic structures at the northeastern margin of the Bohemian Massif (southwestern Poland and northern Czechia)
The analysis of slip tendency of major tectonic faults in Germany
Earthquake ruptures and topography of the Chilean margin controlled by plate interface deformation
Late Quaternary faulting in the southern Matese (Italy): implications for earthquake potential and slip rate variability in the southern Apennines
Rare earth elements associated with carbonatite–alkaline complexes in western Rajasthan, India: exploration targeting at regional scale
Structural complexities and tectonic barriers controlling recent seismic activity in the Pollino area (Calabria–Lucania, southern Italy) – constraints from stress inversion and 3D fault model building
The Mid Atlantic Appalachian Orogen Traverse: a comparison of virtual and on-location field-based capstone experiences
Chronology of thrust propagation from an updated tectono-sedimentary framework of the Miocene molasse (western Alps)
Orogenic lithosphere and slabs in the greater Alpine area – interpretations based on teleseismic P-wave tomography
Ground-penetrating radar signature of Quaternary faulting: a study from the Mt. Pollino region, southern Apennines, Italy
U–Pb dating of middle Eocene–Pliocene multiple tectonic pulses in the Alpine foreland
Detrital zircon provenance record of the Zagros mountain building from the Neotethys obduction to the Arabia–Eurasia collision, NW Zagros fold–thrust belt, Kurdistan region of Iraq
The Subhercynian Basin: an example of an intraplate foreland basin due to a broken plate
Late to post-Variscan basement segmentation and differential exhumation along the SW Bohemian Massif, central Europe
Holocene surface-rupturing earthquakes on the Dinaric Fault System, western Slovenia
Contribution of gravity gliding in salt-bearing rift basins – a new experimental setup for simulating salt tectonics under the influence of sub-salt extension and tilting
Thick- and thin-skinned basin inversion in the Danish Central Graben, North Sea – the role of deep evaporites and basement kinematics
Complex rift patterns, a result of interacting crustal and mantle weaknesses, or multiphase rifting? Insights from analogue models
Interactions of plutons and detachments: a comparison of Aegean and Tyrrhenian granitoids
Insights from elastic thermobarometry into exhumation of high-pressure metamorphic rocks from Syros, Greece
Stress rotation – impact and interaction of rock stiffness and faults
Late Cretaceous to Paleogene exhumation in central Europe – localized inversion vs. large-scale domal uplift
Kinematics and extent of the Piemont–Liguria Basin – implications for subduction processes in the Alps
Effects of basal drag on subduction dynamics from 2D numerical models
Hydrocarbon accumulation in basins with multiple phases of extension and inversion: examples from the Western Desert (Egypt) and the western Black Sea
Long-wavelength late-Miocene thrusting in the north Alpine foreland: implications for late orogenic processes
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
Improving subduction interface implementation in dynamic numerical models
The Bortoluzzi Mud Volcano (Ionian Sea, Italy) and its potential for tracking the seismic cycle of active faults
The Ulakhan fault surface rupture and the seismicity of the Okhotsk–North America plate boundary
Control of increased sedimentation on orogenic fold-and-thrust belt structure – insights into the evolution of the Western Alps
Anticlockwise metamorphic pressure–temperature paths and nappe stacking in the Reisa Nappe Complex in the Scandinavian Caledonides, northern Norway: evidence for weakening of lower continental crust before and during continental collision
Deformation of feldspar at greenschist facies conditions – the record of mylonitic pegmatites from the Pfunderer Mountains, Eastern Alps
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.
Marion Roger, Arjan de Leeuw, Peter van der Beek, Laurent Husson, Edward R. Sobel, Johannes Glodny, and Matthias Bernet
EGUsphere, https://doi.org/10.5194/egusphere-2022-828, https://doi.org/10.5194/egusphere-2022-828, 2022
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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.
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.
Michael Warsitzka, Prokop Závada, Fabian Jähne-Klingberg, and Piotr Krzywiec
Solid Earth, 12, 1987–2020, https://doi.org/10.5194/se-12-1987-2021, https://doi.org/10.5194/se-12-1987-2021, 2021
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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.
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.
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.
Dan Sandiford and Louis Moresi
Solid Earth, 10, 969–985, https://doi.org/10.5194/se-10-969-2019, https://doi.org/10.5194/se-10-969-2019, 2019
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This study investigates approaches to implementing plate boundaries within a fluid dynamic framework, targeted at the evolution of subduction over many millions of years.
Marco Cuffaro, Andrea Billi, Sabina Bigi, Alessandro Bosman, Cinzia G. Caruso, Alessia Conti, Andrea Corbo, Antonio Costanza, Giuseppe D'Anna, Carlo Doglioni, Paolo Esestime, Gioacchino Fertitta, Luca Gasperini, Francesco Italiano, Gianluca Lazzaro, Marco Ligi, Manfredi Longo, Eleonora Martorelli, Lorenzo Petracchini, Patrizio Petricca, Alina Polonia, and Tiziana Sgroi
Solid Earth, 10, 741–763, https://doi.org/10.5194/se-10-741-2019, https://doi.org/10.5194/se-10-741-2019, 2019
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The Ionian Sea in southern Italy is at the center of active convergence between the Eurasian and African plates, with many known
Mw > 7.0 earthquakes. Here, a recently discovered mud volcano (called the Bortoluzzi Mud Volcano or BMV) was surveyed during the Seismofaults 2017 cruise (May 2017). The BMV is the active emergence of crustal fluids probably squeezed up during the seismic cycle. As such, the BMV may potentially be used to track the seismic cycle of active faults.
David Hindle, Boris Sedov, Susanne Lindauer, and Kevin Mackey
Solid Earth, 10, 561–580, https://doi.org/10.5194/se-10-561-2019, https://doi.org/10.5194/se-10-561-2019, 2019
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On one of the least studied boundaries between tectonic plates (North America–Okhotsk in northeastern Russia), which moves very similarly to the famous San Andreas fault in California, we have found the traces of earthquakes from the recent past, but before the time of historical records. This makes us a little more sure that the fault is still the place where movement between the plates takes place, and when it happens again, there could be dangerous earthquakes.
Zoltán Erdős, Ritske S. Huismans, and Peter van der Beek
Solid Earth, 10, 391–404, https://doi.org/10.5194/se-10-391-2019, https://doi.org/10.5194/se-10-391-2019, 2019
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We used a 2-D thermomechanical code to simulate the evolution of an orogen. Our aim was to study the interaction between tectonic and surface processes in orogenic forelands. We found that an increase in the sediment input to the foreland results in prolonged activity of the active frontal thrust. Such a scenario could occur naturally as a result of increasing relief in the orogenic hinterland or a change in climatic conditions. We compare our results with observations from the Alps.
Carly Faber, Holger Stünitz, Deta Gasser, Petr Jeřábek, Katrin Kraus, Fernando Corfu, Erling K. Ravna, and Jiří Konopásek
Solid Earth, 10, 117–148, https://doi.org/10.5194/se-10-117-2019, https://doi.org/10.5194/se-10-117-2019, 2019
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The Caledonian mountains formed when Baltica and Laurentia collided around 450–400 million years ago. This work describes the history of the rocks and the dynamics of that continental collision through space and time using field mapping, estimated pressures and temperatures, and age dating on rocks from northern Norway. The rocks preserve continental collision between 440–430 million years ago, and an unusual pressure–temperature evolution suggests unusual tectonic activity prior to collision.
Felix Hentschel, Claudia A. Trepmann, and Emilie Janots
Solid Earth, 10, 95–116, https://doi.org/10.5194/se-10-95-2019, https://doi.org/10.5194/se-10-95-2019, 2019
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We used microscopy and electron backscatter diffraction to analyse the deformation behaviour of feldspar at greenschist facies conditions in mylonitic pegmatites of the Austroalpine basement. There are strong uncertainties about feldspar deformation, mainly because of the varying contributions of different deformation processes. We observed that deformation is mainly the result of coupled fracturing and dislocation glide, followed by growth and granular flow.
Cited articles
Aldega, L., Viola, G., Casas-Sainz, A., Marcén, M., Román-Berdiel,
T., and van der Lelij, R.: Unraveling Multiple Thermotectonic Events
Accommodated by Crustal-Scale Faults in Northern Iberia, Spain: Insights From
K-Ar Dating of Clay Gouges, Tectonics, 38, 3629–3651,
https://doi.org/10.1029/2019TC005585, 2019. a, b
Aurell, M., Fregenal-Martínez, M., Bádenas, B.,
Muñoz-García, M. B., Élez, J., Meléndez, N., and
de Santisteban, C.: Middle Jurassic–Early Cretaceous tectono-sedimentary
evolution of the southwestern Iberian Basin (central Spain): Major
palaeogeographical changes in the geotectonic framework of the Western
Tethys, Earth-Sci. Rev., 199, 102983,
https://doi.org/10.1016/j.earscirev.2019.102983, 2019. a, b, c, d, e
Avedik, F.: Seismic Structure of the Western Approaches and the South
Armorican Continental Shelf and Its Geological Interpretation., Geol, 1,
29–43, 1975. a
Azambre, B., Rossy, M., and Lago, M.: Caractéristiques
pétrologiques des dolérites tholéiitiques d ' âge
triasique ( ophites ) du domaine pyrénéen, B.
Minéral., 110, 379–396, 1987. a
Balkwill, H. R. and Legall, F. D.: Whale Basin, Offshore Newfoundland:
Extension and Salt Diapirism, chap. 15, North American Margins, 1989. a
Bestani, L., Espurt, N., Lamarche, J., Bellier, O., and Hollender, F.:
Reconstruction of the Provence Chain evolution, southeastern France,
Tectonics, 35, 1506–1525, https://doi.org/10.1002/2016TC004115, 2016. a
Bill, M., O'Dogherty, L., Guex, J., Baumgartner, P. O., and Masson, H.:
Radiolarite ages in Alpine-Mediterranean ophiolites: Constraints on the
oceanic spreading and the Tethys-Atlantic connection, B.
Geol. Soc. Am., 113, 129–143,
https://doi.org/10.1130/0016-7606(2001)113<0129:RAIAMO>2.0.CO;2, 2001. a
Biteau, J. J., Le Marrec, A., Le Vot, M., and Masset, J. M.: The Aquitaine Basin, Petroleum Geoscience, 12, 247–273, https://doi.org/10.1144/1354-079305-674, 2006. a
Bronner, A., Sauter, D., Manatschal, G., Péron-pinvidic, G., and Munschy,
M.: Magmatic breakup as an explanation for magnetic anomalies at magma-poor
rifted margins, Nat. Geosci., 4, 549–553, https://doi.org/10.1038/nphys1201,
2011. a
Brunet, M. F.: Subsidence history of the Aquitaine basin determined from subsidence curves, Geol. Mag., 121, 421–428, https://doi.org/10.1017/S0016756800029952, 1984. a, b, c
Cámara, P.: Salt and Strike-Slip Tectonics as Main Drivers in the Structural Evolution of the Basque-Cantabrian Basin, Spain, in: Permo-Triassic Salt Provinces of Europe, North Africa and the Atlantic Margins, edited by: Soto, J. I., Flinch, J. F., and Gabor, B., Elsevier, 371–393, https://doi.org/10.1016/B978-0-12-809417-4.00018-5, 2017.
Cámara, P. and Flinch, J.: The southern Pyrenees: a salt-based fold-and-thrust belt, in: Permo-Triassic Salt Provinces of Europe, North Africa and the Atlantic Margins, edited by: Soto, J. I., Flinch, J. F., and Gabor, B., Elsevier, 395–415, https://doi.org/10.1016/B978-0-12-809417-4.00019-7, 2017. a, b, c, d
Cerbiá, J. M., López-Ruiz, J., Doblas, M., Martins, L. T., and
Munha, J.: Geochemistry of the Early Jurassic Messejana-Plasencia dyke
(Portugal-Spain); Implications on the Origin of the Central Atlantic Magmatic
Province, J. Petrol., 44, 547–568,
https://doi.org/10.1093/petrology/44.3.547,
2003. a
Channell, J. E. and Kozur, H. W.: How many oceans? Meliata, Vardar, Pindos
oceans in Mesozoic Alpine paleogeography, Geology, 25, 183–186,
https://doi.org/10.1130/0091-7613(1997)025<0183:HMOMVA>2.3.CO;2, 1997. a, b
Chevrot, S., Sylvander, M., Diaz, J., Martin, R., Mouthereau, F., Manatschal,
G., Masini, E., Calassou, S., Grimaud, F., Pauchet, H., and Ruiz, M.: The
non-cylindrical crustal architecture of the Pyrenees, Sci. Rep.-UK, 8,
1–8, https://doi.org/10.1038/s41598-018-27889-x, 2018. a
Choukroune, P. and Mattauer, M.: Tectonique des plaques et Pyrenees; sur le
fonctionnement de la faille transformante nord-pyreneenne; comparaisons avec
des modeles actuels, B. Soc. Géol.
Fr., 7, 689–700, 1978. a
Coltice, N., Bertrand, H., Rey, P., Jourdan, F., Phillips, B. R., and Ricard,
Y.: Global warming of the mantle beneath continents back to the Archaean,
Gondwana Res., 15, 254–266, https://doi.org/10.1016/j.gr.2008.10.001,
2009. a
Curnelle, R.: Evolution structuro-sedimentaire du Trias et de l'Infra-Lias d'Aquitaine., Bulletin des Centres de Recherches Exploration-Production Elf-Aquitaine, 7, 69–99, 1983. a
Debroas, E. J.: Modèle de bassin triangulaire à l'intersection de
décrochements divergents pour le fossé albo-cénomanien de
la Ballongue (Zone Nord-Pyrénéenne, France), B.
Soc. Géol. Fr., 8, 887–898, 1987. a
Debroas, E. J.: Le Flysch noir albo-cénomanien témoin de la
structuration albienne à sénonienne de la Zone
nord-pyrénéenne en Bigorre (Hautes-Pyrénées,
France), B. Soc. Géol. Fr., 8, 273–285, 1990. a
Denèle, Y., Paquette, J. L., Olivier, P., and Barbey, P.: Permian
granites in the Pyrenees: The Aya pluton (Basque Country), Terra Nova, 24,
105–113, https://doi.org/10.1111/j.1365-3121.2011.01043.x, 2012. a
Denèle, Y., Laumonier, B., Paquette, J. L., Olivier, P., Gleizes, G., and
Barbey, P.: Timing of granite emplacement, crustal flow and gneiss dome
formation in the Variscan segment of the Pyrenees, Geol. Soc.
Spec. Publ., 405, 265–287, https://doi.org/10.1144/SP405.5, 2014. a
Deptuck, M. E. and Kendell, K. L.: A review of Mesozoic-Cenozoic salt
tectonics along the Scotian margin, eastern Canada, in: Permo-Triassic Salt
Provinces of Europe, North Africa and the Atlantic Margins,
Elsevier, 287–312, 2017. a
de Saint Blanquat, M.: La faille normale ductile du massif du Saint
Barthélémy. Evolution hercynienne des massifs
nord-pyrénéens catazonaux considérée du point de vue
de leur histoire thermique, Geodin. Acta, 6, 59–77, 1993. a
De Saint Blanquat, M., Lardeaux, J. M., and Brunel, M.: Petrological
arguments for high-temperature extensional deformation in the Pyrenean
Variscan crust (Saint Barthélémy Massif, Ariège, France),
Tectonophysics, 177, 245–262, 1990. a
De Vicente, G., Cloetingh, S. A., Van Wees, J. D., and Cunha, P. P.:
Tectonic classification of Cenozoic Iberian foreland basins,
Tectonophysics, 502, 38–61, https://doi.org/10.1016/j.tecto.2011.02.007,
2011. a
Domeier, M. and Torsvik, T. H.: Plate tectonics in the late Paleozoic,
Geosci. Front., 5, 303–350, https://doi.org/10.1016/j.gsf.2014.01.002,
2014. a
Doré, A. G.: The structural foundation and evolution of Mesozoic seaways
between Europe and the Arctic, Palaeogeogr. Palaeocl., 87, 441–492, 1991. a
Doré, A. G., Lundin, E. R., Jensen, L. N., Birkeland, Ø., Eliassen,
P. E., and Fichler, C.: Principal tectonic events in the evolution of the
northwest European Atlantic margin, in: Geological society, London,
petroleum geology conference series, Geological Society
of London, 5, 41–61, 1999. a
Duretz, T., Asti, R., Lagabrielle, Y., Brun, J. P., Jourdon, A., Clerc, C., and
Corre, B.: Numerical modelling of Cretaceous Pyrenean Rifting: The
interaction between mantle exhumation and syn-rift salt tectonics, Basin
Res., 1–16, https://doi.org/10.1111/bre.12389, 2019. a
Espurt, N., Angrand, P., Teixell, A., Labaume, P., Ford, M., De Saint
Blanquat, M., and Chevrot, S.: Crustal-scale balanced cross-section and
restorations of the Central Pyrenean belt (Nestes-Cinca transect):
Highlighting the structural control of Variscan belt and Permian-Mesozoic
rift systems on mountain building, Tectonophysics, 764, 25–45,
https://doi.org/10.1016/j.tecto.2019.04.026, 2019. a
Etheve, N., Mohn, G., Frizon de Lamotte, D., Roca, E., Tugend, J., and
Gómez-Romeu, J.: Extreme Mesozoic Crustal Thinning in the Eastern
Iberia Margin: The Example of the Columbrets Basin (Valencia Trough),
Tectonics, 37, 636–662, https://doi.org/10.1002/2017TC004613, 2018. a
Evans, D.: The Millennium Atlas: Petroleum Geology of the Central and Northern North Sea, Geological Society of London, London, 2003. a
Fabriès, J., Lorand, J. P., Bodinier, J. L., and Dupuy, C.: Evolution of
the upper mantle beneath the pyrenees: Evidence from orogenic spinel
lherzolite massifs, J. Petrol., 55–76,
https://doi.org/10.1093/petrology/Special_Volume.2.55, 1991. a
Fabriès, J., Lorand, J. P., and Bodinier, J. L.: Petrogenetic evolution
of orogenic lherzolite massifs in the central and western Pyrenees,
Tectonophysics, 292, 145–167, https://doi.org/10.1016/S0040-1951(98)00055-9, 1998. a
Fernández, O.: The Jurassic evolution of the Africa-Iberia conjugate
margin and its implications on the evolution of the Atlantic-Tethys triple
junction, Tectonophysics, 750, 379–393, https://doi.org/10.1016/j.tecto.2018.12.006, 2019. a, b
Ferrer, O., Jackson, M. P., Roca, E., and Rubinat, M.: Evolution of salt
structures during extension and inversion of the Offshore Parentis Basin
(Eastern Bay of Biscay), Geol. Soc. Spec. Publ., 363,
361–380, https://doi.org/10.1144/SP363.16, 2012. a
Ganne, J., Feng, X., Rey, P., and De Andrade, V.: Statistical petrology
reveals a link between supercontinents cycle and mantle global climate,
Am. Mineral., 101, 2768–2773, https://doi.org/10.2138/am-2016-5868,
2016. a
Glennie, K. W., Higham, J., and Stemmerik, L.: Permian, in: The millennium
atlas; petroleum geology of the central and northern North Sea, edited by:
Evans, D., Graham, C., Armour, A., and Bathurst, P., chap. 8, 91–103,
Geological Society of London, London, 2003. a
Golberg, J. M. and Leyreloup, A. F.: High temperature-low pressure Cretaceous metamorphism related to crustal thinning (Eastern North Pyrenean Zone, France), Contributions to Mineralogy and Petrology, 104, 194–207, https://doi.org/10.1007/BF00306443, 1990. a
Goldsmith, P. J., Hudson, G., and Van Veen, P.: Triassic, in: The
millennium atlas; petroleum geology of the central and northern North Sea,
edited by: Evans, D., Graham, C., Armour, A., and Bathurst, P., 105–127,
Geological Society of London, London, 2003. a
Grool, A. R., Huismans, R. S., and Ford, M.: Salt décollement and rift
inheritance controls on crustal deformation in orogens, Terra Nova, 31,
562–568, https://doi.org/10.1111/ter.12428, 2019. a
Hafid, M.: Triassic-early Liassic extensional systems and their Tertiary
inversion, Essaouira Basin (Morocco), Mar. Petrol. Geol., 17,
409–429, https://doi.org/10.1016/S0264-8172(98)00081-6, 2000. a
Handy, M. R., M. Schmid, S., Bousquet, R., Kissling, E., and Bernoulli, D.:
Reconciling plate-tectonic reconstructions of Alpine Tethys with the
geological-geophysical record of spreading and subduction in the Alps,
Earth-Sci. Rev., 102, 121–158, https://doi.org/10.1016/j.earscirev.2010.06.002,
2010. a, b, c, d, e
Hanne, D., White, N., and Lonergan, L.: Subsidence analyses from the Betic
Cordillera, southeast Spain, Basin Res., 15, 1–21,
https://doi.org/10.1046/j.1365-2117.2003.00192.x, 2003. a, b
Hassaan, M., Inge, J., Helge, R., and Tsikalas, F.: Carboniferous graben structures , evaporite accumulations and tectonic inversion in the southeastern Norwegian Barents Sea, Marine and Petroleum Geology, 112, 104038, https://doi.org/10.1016/j.marpetgeo.2019.104038, 2019. a
Hassaan, M., Inge, J., Helge, R., and Tsikalas, F.: Carboniferous graben
structures, evaporite accumulations and tectonic inversion in the
southeastern Norwegian Barents Sea, Mar. Petrol. Geol., 112,
104038, https://doi.org/10.1016/j.marpetgeo.2019.104038, 2020. a, b
Heeremans, M., Timmerman, M. J., Kirstein, L. A., and Faleide, J. I.: New
constraints on the timing of late Carboniferous-early Permian volcanism in
the central North Sea, Geol. Soc. Spec. Publ.,
223, 177–193, 2004. a
Heine, C., Zoethout, J., and Müller, R. D.: Kinematics of the South Atlantic rift, Solid Earth, 4, 215–253, https://doi.org/10.5194/se-4-215-2013, 2013. a
Jackson, C. A., Gawthorpe, R. L., Elliott, G. M., and Rogers, E. R.: Salt
thickness and composition influence rift structural style, northern North
Sea, offshore Norway, 514–538, https://doi.org/10.1111/bre.12332, 2019. a, b, c
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, 1–24,
https://doi.org/10.1029/2008TC002406, 2009. a, b, c, d
Jourdon, A., Mouthereau, F., Pourhiet, L. L., and Callot, J. P.: Topographic
and Tectonic Evolution of Mountain Belts Controlled by Salt Thickness and
Rift Architecture, 39, 1–14, https://doi.org/10.1029/2019TC005903, 2020. a
Kneller, E. A., Johnson, C. A., Karner, G. D., Einhorn, J., and Queffelec, T. A.: Inverse methods for modeling non-rigid plate kinematics: Application to mesozoic plate reconstructions of the Central Atlantic, Comput. Geosci., 49, 217–230, https://doi.org/10.1016/j.cageo.2012.06.019, 2012. a
Labails, C., Olivet, J. L., Aslanian, D., and Roest, W. R.: An alternative
early opening scenario for the Central Atlantic Ocean, Earth Planet.
Sc. Lett., 297, 355–368, https://doi.org/10.1016/j.epsl.2010.06.024,
2010. a
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, 1–26, https://doi.org/10.1029/2009TC002588, 2010. a, b, c
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, b
Lago, M., Arranz, E., Pocoví, A., Galé, C., and Gil-Imaz, A.:
Lower Permian magmatism of the Iberian Chain, Central Spain, and its
relationship to extensional tectonics, Geol. Soc. Spec.
Publ., 223, 465–490, https://doi.org/10.1144/GSL.SP.2004.223.01.20,
2004a. a
Lago, M., Arranz, E., Pocoví, A., Galé, C., and Gil-Imaz, A.:
Permian magmatism and basin dynamics in the southern Pyrenees: a record of
the transition from late Variscan transtension to early Alpine extension,
Geol. Soc. Spec. Publ., 223, 439–464,
2004b. a
Leleu, S., Hartley, A. J., van Oosterhout, C., Kennan, L., Ruckwied, K., and
Gerdes, K.: Structural, stratigraphic and sedimentological characterisation
of a wide rift system: The Triassic rift system of the Central Atlantic
Domain, Earth-Sci. Rev., 158, 89–124,
https://doi.org/10.1016/j.earscirev.2016.03.008, 2016. a, b, c, d, e
Malavieille, J., Guihot, P., Costa, S., Lardeaux, J. M., and Gardien, V.:
Collapse of the thickened Variscan crust in the French Massif Central: Mont
Pilat extensional shear zone and St. Etienne Late Carboniferous basin,
Tectonophysics, 177, 139–149, 1990. a
Marroni, M., Meneghini, F., and Pandolfi, L.: A Revised Subduction Inception
Model to Explain the Late Cretaceous, Double-Vergent Orogen in the
Precollisional Western Tethys: Evidence From the Northern Apennines,
Tectonics, 36, 2227–2249, https://doi.org/10.1002/2017TC004627, 2017. a
Marzoli, A., Renne, P. R., Piccirillo, E. M., Ernesto, M., Bellieni, G., and
De Min, A.: Extensive 200-million-year-old continental flood basalts of
the Central Atlantic Magmatic Province, Science, 284, 616–618,
https://doi.org/10.1126/science.284.5414.616, 1999. a, b
Masini, E., Manatschal, G., Tugend, J., Mohn, G., and Flament, J. M.: The
tectono-sedimentary evolution of a hyper-extended rift basin: The example of
the Arzacq-Mauléon rift system (Western Pyrenees, SW France),
Int. J. Earth Sci., 103, 1569–1596,
https://doi.org/10.1007/s00531-014-1023-8, 2014. a
McHone, J. G.: Non-plume magmatism and rifting during the opening of the
central Atlantic Ocean, Tectonophysics, 316, 287–296,
https://doi.org/10.1016/S0040-1951(99)00260-7, 2000. a, b
McKenzie, D.: Some remarks on the development of sedimentary basins, Earth
Planet. Sc. Lett., 40, 25–32,
https://doi.org/10.1016/0012-821X(78)90071-7, 1978. a
McKenzie, D., Daly, M. C., and Priestley, K.: The lithospheric structure of
Pangea, Geology, 43, 783–786, https://doi.org/10.1130/G36819.1, 2015. a
McQuarrie, N. and Van Hinsbergen, D. J.: Retrodeforming the Arabia-Eurasia
collision zone: Age of collision versus magnitude of continental subduction,
Geology, 41, 315–318, https://doi.org/10.1130/G33591.1, 2013. a
Mohn, G., Karner, G. D., Manatschal, G., and Johnson, C. A.: Structural and
stratigraphic evolution of the Iberia-Newfoundland hyper-extended rifted
margin: A quantitative modelling approach, Geol. Soc. Spec.
Publ., 413, 53–89, https://doi.org/10.1144/SP413.9, 2015. a, b
Mouthereau, F., Filleaudeau, P. Y., Vacherat, A., Pik, R., Lacombe, O., Fellin,
M. G., Castelltort, S., Christophoul, F., and Masini, E.: Placing limits to
shortening evolution in the Pyrenees: Role of margin architecture and
implications for the Iberia/Europe convergence, Tectonics, 33, 2283–2314,
https://doi.org/10.1002/2014TC003663, 2014. a, b, c
Müller, D. R., Cannon, J., Qin, X., Watson, R. J., Gurnis, M., Williams,
S., Pfaffelmoser, T., Seton, M., Russell, S. H., and Zahirovic, S.: GPlates:
Building a Virtual Earth Through Deep Time, Geochem. Geophy.
Geosy., 19, 2243–2261, https://doi.org/10.1029/2018GC007584, 2018. a, b
Müller, D. R., Zahirovic, S., Williams, S. E., Cannon, J., Seton, M.,
Bower, D. J., Tetley, M. G., Heine, C., Le Breton, E., Liu, S., Russell,
S. H., Yang, T., Leonard, J., and Gurnis, M.: A Global Plate Model Including
Lithospheric Deformation Along Major Rifts and Orogens Since the Triassic,
Tectonics, 38, 1884–1907, https://doi.org/10.1029/2018TC005462, 2019. a, b, c
Müller, R. D., Sdrolias, M., Gaina, C., and Roest, W. R.: Age, spreading
rates, and spreading asymmetry of the world's ocean crust, Geochem.
Geophy. Geosy., 9, 1–19, https://doi.org/10.1029/2007GC001743, 2008. a
Nirrengarten, M., Manatschal, G., Tugend, J., Kusznir, N. J., and Sauter, D.:
Nature and origin of the J-magnetic anomaly offshore Iberia–Newfoundland:
implications for plate reconstructions, Terra Nova, 29, 20–28,
https://doi.org/10.1111/ter.12240, 2017. a
Olsen, P. E.: Stratigraphic Record of the Early Mesozoic Breakup of Pangea in
the Laurasia-Gondwana Rift System, Annu. Rev. Earth Pl.
Sc., 25, 337–401, https://doi.org/10.1146/annurev.earth.25.1.337, 1997. a, b
Olyphant, J. R., Johnson, R. A., and Hughes, A. N.: Evolution of the Southern
Guinea Plateau: Implications on Guinea-Demerara Plateau formation using
insights from seismic, subsidence, and gravity data, Tectonophysics, 717,
358–371, https://doi.org/10.1016/j.tecto.2017.08.036, 2017. a
Omodeo-Salé, S., Salas, R., Guimerà, J., Ondrak, R., Mas, R.,
Arribas, J., Suárez-Ruiz, I., and Martinez, L.: Subsidence and thermal
history of an inverted Late Jurassic-Early Cretaceous extensional basin
(Cameros, North-central Spain) affected by very low- to low-grade
metamorphism, Basin Res., 29, 156–174, https://doi.org/10.1111/bre.12142, 2017. a
Ortí, F., Pérez-López, A., and Salvany, J. M.: Triassic
evaporites of Iberia: Sedimentological and palaeogeographical implications
for the western Neotethys evolution during the Middle Triassic–Earliest
Jurassic, Palaeogeogr. Palaeocl., 471, 157–180,
https://doi.org/10.1016/j.palaeo.2017.01.025, 2017. a, b
Peace, A. L., Phethean, J., Franke, D., Foulger, G., Schiffer, C., Welford, J.,
McHone, G., Rocchi, S., Schnabel, M., and Doré, A.: A review of
Pangaea dispersal and Large Igneous Provinces – In search of a causative
mechanism, Earth-Sci. Rev., p. 102902,
https://doi.org/10.1016/j.earscirev.2019.102902, 2019a. a, b, c
Peace, A. L., Welford, J. K., Ball, P. J., and Nirrengarten, M.: Deformable
plate tectonic models of the southern North Atlantic, J.
Geodyn., 128, 11–37, https://doi.org/10.1016/j.jog.2019.05.005,
2019b. a, b, c
Pereira, R., Alves, T. M., and Mata, J.: Alternating crustal architecture in
West Iberia: A review of its significance in the context of NE atlantic
rifting, J. Geol. Soc., 174, 522–540,
https://doi.org/10.1144/jgs2016-050, 2017. a
Phillips, T. B., Jackson, C. A.-L., Bell, R. E., and Duffy, O. B.: Oblique reactivation of lithosphere-scale lineaments controls rift physiography – the upper-crustal expression of the Sorgenfrei–Tornquist Zone, offshore southern Norway, Solid Earth, 9, 403–429, https://doi.org/10.5194/se-9-403-2018, 2018. a
Phillips, T. B., Fazlikhani, H., Gawthorpe, R. L., Fossen, H., Jackson, C. A., Bell, R. E., Faleide, J. I., and Rotevatn, A.: The Influence of Structural Inheritance and Multiphase Extension on Rift Development, the NorthernNorth Sea, Tectonics, 38, 4099–4126, https://doi.org/10.1029/2019TC005756, 2019. a
Puga, E., Fanning, M., Díaz de Federico, A., Nieto, J. M., Beccaluva,
L., Bianchini, G., and Díaz Puga, M. A.: Petrology, geochemistry and
U-Pb geochronology of the Betic Ophiolites: Inferences for Pangaea break-up
and birth of the westernmost Tethys Ocean, Lithos, 124, 255–272,
https://doi.org/10.1016/j.lithos.2011.01.002, 2011. a
Quintana, L., Pulgar, J. A., and Alonso, J. L.: Displacement transfer from borders to interior of a plate: A crustal transect of Iberia, Tectonophysics, 663, 378–398, https://doi.org/10.1016/j.tecto.2015.08.046, 2015 a
Quirk, D. G. and Rüpke, L. H.: Melt-induced buoyancy may explain the
elevated rift-rapid sag paradox during breakup of continental plates,
Sci. Rep.-UK, 8, 1–13, https://doi.org/10.1038/s41598-018-27981-2, 2018. a
Ramos, A., Fernández, O., Terrinha, P., and Muñoz, J. A.:
Extension and inversion structures in the Tethys–Atlantic linkage zone,
Algarve Basin, Portugal, Int. J. Earth Sci., 105,
1663–1679, https://doi.org/10.1007/s00531-015-1280-1, 2016. 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
Salas, R. and Casas, A.: Mesozoic extensional tectonics, stratigraphy and
crustal evolution during the Alpine cycle of the eastern Iberian basin,
Tectonophysics, 228, 33–55, https://doi.org/10.1016/0040-1951(93)90213-4, 1993. a, b
Salas, R., Guimerà, J., Mas, R., Martín-Closas, C., Melendez, A., and Alonso, A.: Evolution of the Mesozoic Central Iberian Rift System and its Cainozoic inversion (Iberian chain), in: Peri-Tethys Memoir 6: Peri-Tethyan Rift/Wrench Basins and Passive Margins, edited by: Ziegler, P. A., Cavazza, W., Robertson, A., and Crasquin-Soleau, S., Paris, Mémoir du Muséum d'Histoire Naturelle edn., 186, 145–186, 2001. a, b, c
Sallarès, V., Martínez-Loriente, S., Prada, M., Gràcia, E.,
Ranero, C., Gutscher, M. A., Bartolome, R., Gailler, A., Dañobeitia,
J. J., and Zitellini, N.: Seismic evidence of exhumed mantle rock basement
at the Gorringe Bank and the adjacent Horseshoe and Tagus abyssal plains (SW
Iberia), Earth Planet. Sci. Lett., 365, 120–131,
https://doi.org/10.1016/j.epsl.2013.01.021, 2013. a
Sánchez-Navas, A., García-Casco, A., Mazzoli, S., and
Martín-Algarra, A.: Polymetamorphism in the Alpujarride Complex, Betic
Cordillera, South Spain, J. Geol., 125, 637–657,
https://doi.org/10.1086/693862, 2017. a
Sandoval, L., Welford, J. K., MacMahon, H., and Peace, A. L.: Determining
continuous basins across conjugate margins: The East Orphan, Porcupine, and
Galicia Interior basins of the southern North Atlantic Ocean, Mar.
Petrol. Geol., 110, 138–161, https://doi.org/10.1016/j.marpetgeo.2019.06.047,
2019. a, b
Saspiturry, N., Cochelin, B., Razin, P., Leleu, S., Lemirre, B., Bouscary, C., Issautier, B., Serrano, O., Lasseur, E., Baudin, T., and Allanic, C.: Tectono-sedimentary evolution of a rift system controlled by Permian post-orogenic extension and metamorphic core complex formation (Bidarray Basin and Ursuya dome, Western Pyrenees), Tectonophysics, 768, 228180, https://doi.org/10.1016/j.tecto.2019.228180, 2019. a, b, c
Schaltegger, U., Desmurs, L., Manatschal, G., Müntener, O., Meier, M.,
Frank, M., and Bernoulli, D.: The transition from rifting to sea‐floor
spreading within a magma‐poor rifted margin: Field and isotopic
constraints, Terra Nova, 14, 156–162, 2002. a
Schettino, A. and Turco, E.: Breakup of Pangaea and plate kinematics of the central Atlantic and Atlas regions, Geophys. J. Int., 178, 1078–1097, https://doi.org/10.1111/j.1365-246X.2009.04186.x, 2009. a
Schettino, A. and Turco, E.: Tectonic history of the Western Tethys since the
Late Triassic, B. Geol. Soc. Am., 123, 89–105,
https://doi.org/10.1130/B30064.1, 2011. a
Schmid, S. M., Bernoulli, D., Fügenschuh, B., Matenco, L., Schefer, S.,
Schuster, R., Tischler, M., and Ustaszewski, K.: The
Alpine-Carpathian-Dinaridic orogenic system: Correlation and evolution of
tectonic units, Swiss J. Geosci., 101, 139–183,
https://doi.org/10.1007/s00015-008-1247-3, 2008. a, b, c, d, e, f
Scisciani, V. and Esestime, P.: The Triassic evaporites in the evolution of
the Adriatic Basin, in: Permo-Triassic Salt Provinces of Europe, North
Africa and the Atlantic Margins, Elsevier, 499–516, 2017. a
Serrano, O., Delmas, J., Hanot, F., Vially, R., Herbin, J.-P., Houel, P., and Tourlière, B.: Le Bassin d’Aquitaine: valorisation des données sismiques, cartographie structurale et potentiel pétrolier, Tech. rep., BRGM & IFP, Orléans, 2006. a
Seton, M., Müller, R. D., Zahirovic, S., Gaina, C., Torsvik, T. H.,
Shephard, G. E., Talsma, A., Gurnis, M., Turner, M., Maus, S., and Chandler,
M.: Global continental and ocean basin reconstructions since 200 Ma,
Earth-Sci. Rev., 113, 212–270, https://doi.org/10.1016/j.earscirev.2012.03.002, 2012. a, b
Sibuet, J. C., Srivastava, S. P., and Spakman, W.: Pyrenean orogeny and plate
kinematics, J. Geophys. Res.-Sol. Ea., 109, 1–18,
https://doi.org/10.1029/2003JB002514, 2004. a, b, c, d
Silver, P. G., Behn, M. D., Kelley, K., Schmitz, M., and Savage, B.:
Understanding cratonic flood basalts, Earth Planet. Sc. Lett.,
245, 190–201, https://doi.org/10.1016/j.epsl.2006.01.050, 2006. a, b
Simon, N. S. and Podladchikov, Y. Y.: The effect of mantle composition on
density in the extending lithosphere, Earth Planet. Sc. Lett.,
272, 148–157, https://doi.org/10.1016/j.epsl.2008.04.027, 2008. a
Solé, J., Cosca, M., Sharp, Z., and Enrique, P.: 40Ar∕39Ar
Geochronology and stable isotope geochemistry of Late-Hercynian intrusions
from north-eastern Iberia with implications for argon loss in K-feldspar,
Int. J. Earth Sci., 91, 865–881,
https://doi.org/10.1007/s00531-001-0251-x, 2002. a
Sopeña, A., López, J., Arche, A., Pérez-Arlucea, M., Ramos,
A., Virgili, C., and Hernando, S.: Permian and Triassic rift basins of the
Iberian Peninsula, in: Developments in Geotectonics, 22, 757–786,
https://doi.org/10.1016/B978-0-444-42903-2.50036-1,
1988. a, b
Soto, R., Casas-Sainz, A. M., Oliva-Urcia, B., García-Lasanta, C.,
Izquierdo-Llavall, E., Moussaid, B., Kullberg, J. C., Román-Berdiel,
T., Sánchez-Moya, Y., Sopeña, A., Torres-López, S.,
Villalaín, J. J., El-Ouardi, H., Gil-Peña, I., and Hirt, A. M.:
Triassic stretching directions in Iberia and North Africa inferred from
magnetic fabrics, Terra Nova, 31, 465–478, https://doi.org/10.1111/ter.12416, 2019. a, b, c, d, e, f
Spooner, C., Stephenson, R., and Butler, R. W.: Pooled subsidence records from
numerous wells reveal variations in pre-break-up rifting along the proximal
domains of the Iberia-Newfoundland continental margins, Geol. Mag.,
156, 1323–1333, https://doi.org/10.1017/S0016756818000651, 2019. a, b, c
Stampfli, G. M. and Borel, G. D.: A plate tectonic model for the Paleozoic and
Mesozoic constrained by dynamic plate boundaries and restored synthetic
oceanic isochrons, Earth Planet. Sc. Lett., 196, 17–33,
https://doi.org/10.1016/S0012-821X(01)00588-X, 2002. a, b, c, d
Stampfli, G. M., Mosar, J., Favre, P., Pillevuit, A., and Vannay, J.-C.:
Permo-Mesozoic evolution of the western Tethyan realm: the Neotethys/East-
Mediterranean connection, in: Peri-Tethys Memoir 6: Peri-Tethyan Rift/Wrench
Basins and Passive Margins, edited by: Ziegler, P. A., Cavazza, W., Robertson,
A. H. F., and Crasquin-Soleau, S., Mémoirs du
Muséum d'Histoire Naturelle, Paris, 186, 51–108, 2001. a, b, c
Srivastava, S. P., Sibuet, J. C., Cande, S., Roest, W. R., and Reid, I. D.: Magnetic evidence for slow seafloor spreading during the formation of the Newfoundland and Iberian margins, Earth Planet. Sc. Lett., 182, 61–76, https://doi.org/10.1016/S0012-821X(00)00231-4, 2000. a
Tankard, A. J. and Welsink, H. J.: Extensional tectonics and stratigraphy of
Hibernia oil field, Grand Banks, Newfoundland, AAPG Bulletin, 71,
1210–1232, 1987. a
Tavani, S. and Granado, P.: Along-strike evolution of folding, stretching and
breaching of supra-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. a
Tavani, S., Quintà, A., and Granado, P.: Tectonophysics Cenozoic
right-lateral wrench tectonics in the Western Pyrenees (Spain): The Ubierna
Fault System, Tectonophysics, 509, 238–253,
https://doi.org/10.1016/j.tecto.2011.06.013, 2011. a, b, c
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. Revi., 187, 314–337, https://doi.org/10.1016/j.earscirev.2018.10.008,
2018. a, b, c, d
Thinon, I., Fidalgo-González, L., Réhault, J. P., and Olivet, J. L.: Déformations pyrénéennes dans le golfe de Gascogne, Comptes Rendus de l’Academie de Sciences – Serie IIa: Sciences de la Terre et des Planetes, 332, 561–568, https://doi.org/10.1016/S1251-8050(01)01576-2, 2001. a
Thinon, I., Réhault, J. P., and Fidalgo-González, L.: La couverture sédimentaire syn-rift de la marge Nord-Gascogne et du Bassin armoricain (golfe de Gascogne): à partir de nouvelles données de sismique réflexion, Bulletin de la Societe Geologique de France, 173, 515–522, https://doi.org/10.2113/173.6.515, 2002. a
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. a, b
Tugend, J., Manatschal, G., and Kusznir, N. J.: Spatial and temporal evolution
of hyperextended rift systems: Implication for the nature, kinematics, and
timing of the Iberian- European plate boundary, Geology, 43, 15–18,
https://doi.org/10.1130/G36072.1, 2015. a, b, c, d
Tugend, J., Chamot-Rooke, N., Arsenikos, S., Blanpied, C., and Frizon de
Lamotte, D.: Geology of the Ionian Basin and Margins: A Key to the East
Mediterranean Geodynamics, Tectonics, 38, 2668–2702,
https://doi.org/10.1029/2018TC005472, 2019. a, b
Vacherat, A., Mouthereau, F., Pik, R., Huyghe, D., Paquette, J. L.,
Christophoul, F., Loget, N., and Tibari, B.: Rift-to-collision sediment
routing in the Pyrenees: A synthesis from sedimentological, geochronological
and kinematic constraints, Earth-Sci. Rev., 172, 43–74,
https://doi.org/10.1016/j.earscirev.2017.07.004, 2017. a
van Hinsbergen, D. J., Torsvik, T. H., Schmid, S. M.,
Maţenco,
L. C., Maffione, M., Vissers, R. L., Gürer, D., and Spakman, W.: Orogenic architecture of the Mediterranean region and kinematic reconstruction of its tectonic evolution since the Triassic, Gondwana Research, 81, 79–229, https://doi.org/10.1016/j.gr.2019.07.009, 2020. a, b, c, d, e
Van Wees, J. D., Arche, A., Beijdorff, C. G., López-Gómez, J.,
and Cloetingh, S. A.: Temporal and spatial variations in tectonic subsidence
in the Iberian Basin (eastern Spain): Inferences from automated forward
modelling of high-resolution stratigraphy (Permian-Mesozoic),
Tectonophysics, 300, 285–310, https://doi.org/10.1016/S0040-1951(98)00244-3, 1998. a
Van Wees, J. D., Stephenson, R., Ziegler, P. A., Bayer, U., McCann, T.,
Dadlez, R., Gaupp, R., Narkiewicz, M., Bitzer, F., and Scheck, M.: On the
origin of the southern Permian Basin, Central Europe, Mar. Petrol.
Geol., 17, 43–59, 2000. a
Vargas, H., Gaspar-Escribano, J. M., López-Gómez, J., Van Wees, J. D., Cloetingh, S., de La Horra, R., and Arche, A.: A comparison of the Iberian and Ebro Basins during the Permian and Triassic, eastern Spain: A quantitative subsidence modelling approach, Tectonophysics, 474, 160–183, https://doi.org/10.1016/j.tecto.2008.06.005, 2009. a
Vergés, J., Poprawski, Y., Almar, Y., Drzewiecki, P. A., Moragas, M., Bover-Arnal, T., Macchiavelli, C., Wright, W., Messager, G., Embry, J., and Hunt, D.: Tectono-sedimentary evolution of Jurassic–Cretaceous diapiric structures: Miravete anticline, Maestrat Basin, Spain, Basin Res., https://doi.org/10.1111/bre.12447, online first, 2020. a
Vielzeuf, D. and Kornprobst, J.: Crustal splitting and the emplacement of Pyrenean lherzolites and granulites – A reply to M. W. Fischer, Earth Planet. Sc. Lett., 70, 439–443, https://doi.org/10.1016/0012-821X(84)90028-1, 1984. a
Vissers, R.: Variscan extension in the Pyrenees, Tectonics, 11, 1369–1384,
1992. a
Vissers, R. and Meijer, P.: Mesozoic rotation of Iberia: Subduction in the
Pyrenees?, Earth-Sci. Rev., 110, 93–110,
https://doi.org/10.1016/j.earscirev.2011.11.001, 2012. a, b, c, d
Watts, A. B.: Isostasy and Flexure of the Lithosphere, Cambridge University
Press, 2001. a
Welsink, H. J., Dwyer, J. D., and Knight, R. J.: Tectono-Stratigraphy of the
Passive Margin Off Nova Scotia, chap. 14, North American Margins, 1989. a
Whitmarsh, R. B. and Manatschal, G.: Evolution of magma poor continental margins: from rifting to the onset of seafloor spreading, in: Regional Geology and Tectonics: Phanerozoic Passive Margins, Cratonic Basins and Global Tectonic Maps, edited by: Roberts, D. and Bally, A. W., chap. 9, Elsevier, 326–341, https://doi.org/10.1016/B978-0-444-56357-6.00008-1, 2012. a
Ziegler, P. A.: Geodynamic model for Alpine intra-plate compressional
deformation in Western and Central Europe, in: Inversion Tectonics, edited
by: Cooper, M. A. and Williams, G. D., Geol. Soc.
Spec. Publ., 3, 63–85, 1989. a
Ziegler, P. A.: Collision related intra-plate compression deformations in
Western and Central Europe, J. Geodyn., 11, 357–388, 1990. a
Ziegler, P. A. and Dèzes, P.: Crustal evolution of Western and Central
Europe, Geol. Soc. Mem., 32, 43–56,
https://doi.org/10.1144/GSL.MEM.2006.032.01.03, 2006.
a
Ziegler, P. A., Schumacher, M. E., Dèzes, P., van Wees, J. D., and
Cloetingh, S. A.: Post-Variscan evolution of the lithosphere in the Rhine
Graben area: Constraints from subsidence modelling, Geol. Soc. Spec. Publ., 223, 289–317, https://doi.org/10.1144/GSL.SP.2004.223.01.13,
2004. a
Short summary
We study the Iberian plate motion, from the late Permian to middle Cretaceous. During this time interval, two oceanic systems opened. Geological evidence shows that the Iberian domain preserved the propagation of these two rift systems well. We use geological evidence and pre-existing kinematic models to propose a coherent kinematic model of Iberia that considers both the Neotethyan and Atlantic evolutions. Our model shows that the Europe–Iberia plate boundary was made of two rift systems.
We study the Iberian plate motion, from the late Permian to middle Cretaceous. During this time...
