Articles | Volume 12, issue 10
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Late to post-Variscan basement segmentation and differential exhumation along the SW Bohemian Massif, central Europe
GeoZentrum Nordbayern, Friedrich-Alexander-Universität (FAU) Erlangen-Nürnberg, Schlossgarten 5, 91054 Erlangen, Germany
GeoZentrum Nordbayern, Friedrich-Alexander-Universität (FAU) Erlangen-Nürnberg, Schlossgarten 5, 91054 Erlangen, Germany
GeoZentrum Nordbayern, Friedrich-Alexander-Universität (FAU) Erlangen-Nürnberg, Schlossgarten 5, 91054 Erlangen, Germany
GeoZentrum Nordbayern, Friedrich-Alexander-Universität (FAU) Erlangen-Nürnberg, Schlossgarten 5, 91054 Erlangen, Germany
GeoZentrum Nordbayern, Friedrich-Alexander-Universität (FAU) Erlangen-Nürnberg, Schlossgarten 5, 91054 Erlangen, Germany
Leibniz-Institut für Angewandte Geophysik, Stilleweg 2, 30655 Hanover, Germany
Institut für Geologie, Leibniz Universität Hannover, Callinstraße 30, 30167 Hanover, Germany
No articles found.
Sonja H. Wadas, Hermann Buness, Raphael Rochlitz, Peter Skiba, Thomas Günther, Michael Grinat, David C. Tanner, Ulrich Polom, Gerald Gabriel, and Charlotte M. Krawczyk
Solid Earth, 13, 1673–1696,Short summary
The dissolution of rocks poses a severe hazard because it can cause subsidence and sinkhole formation. Based on results from our study area in Thuringia, Germany, using P- and SH-wave reflection seismics, electrical resistivity and electromagnetic methods, and gravimetry, we develop a geophysical investigation workflow. This workflow enables identifying the initial triggers of subsurface dissolution and its control factors, such as structural constraints, fluid pathways, and mass movement.
Flavio S. Anselmetti, Milos Bavec, Christian Crouzet, Markus Fiebig, Gerald Gabriel, Frank Preusser, Cesare Ravazzi, and DOVE scientific team
Sci. Dril., 31, 51–70,Short summary
Previous glaciations eroded below the ice deep valleys in the Alpine foreland, which, with their sedimentary fillings, witness the timing and extent of these glacial advance–retreat cycles. Drilling such sedimentary sequences will thus provide well-needed evidence in order to reconstruct the (a)synchronicity of past ice advances in a trans-Alpine perspective. Eventually these data will document how the Alpine foreland was shaped and how the paleoclimate patterns varied along and across the Alps.
Simon Freitag, Michael Drews, Wolfgang Bauer, Florian Duschl, David Misch, and Harald Stollhofen
Solid Earth, 13, 1003–1026,Short summary
The carbonates of the Malm are the main reservoir rocks for hydrothermal heat and power generation in southern Germany. To better understand these buried rocks, the carbonates exposed in northern Bavaria are often investigated. As the petrophysical properties of carbonates strongly depend on their subsidence history and maximum burial depth, we will investigate this issue by analyzing mudstones, which indirectly store this type of information and are found just below the Malm carbonates.
Hamed Fazlikhani, Wolfgang Bauer, and Harald Stollhofen
Solid Earth, 13, 393–416,Short summary
Interpretation of newly acquired FRANKEN 2D seismic survey data in southeeastern Germany shows that upper Paleozoic low-grade metasedimentary rocks and possible nappe units are transported by Variscan shear zones to ca. 65 km west of the Franconian Fault System (FFS). We show that the locations of post-Variscan upper Carboniferous–Permian normal faults and associated graben and half-graben basins are controlled by the geometry of underlying Variscan shear zones.
Tommaso Pivetta, Carla Braitenberg, Franci Gabrovšek, Gerald Gabriel, and Bruno Meurers
Hydrol. Earth Syst. Sci., 25, 6001–6021,Short summary
Gravimetry offers a valid complement to classical hydrologic measurements in order to characterize karstic systems in which the recharge process causes fast accumulation of large water volumes in the voids of the epi-phreatic system. In this contribution we show an innovative integration of gravimetric and hydrologic observations to constrain a hydrodynamic model of the Škocjan Caves (Slovenia). We demonstrate how the inclusion of gravity observations improves the water mass budget estimates.
Pavol Zahorec, Juraj Papčo, Roman Pašteka, Miroslav Bielik, Sylvain Bonvalot, Carla Braitenberg, Jörg Ebbing, Gerald Gabriel, Andrej Gosar, Adam Grand, Hans-Jürgen Götze, György Hetényi, Nils Holzrichter, Edi Kissling, Urs Marti, Bruno Meurers, Jan Mrlina, Ema Nogová, Alberto Pastorutti, Corinne Salaun, Matteo Scarponi, Josef Sebera, Lucia Seoane, Peter Skiba, Eszter Szűcs, and Matej Varga
Earth Syst. Sci. Data, 13, 2165–2209,Short summary
The gravity field of the Earth expresses the overall effect of the distribution of different rocks at depth with their distinguishing densities. Our work is the first to present the high-resolution gravity map of the entire Alpine orogen, for which high-quality land and sea data were reprocessed with the exact same calculation procedures. The results reflect the local and regional structure of the Alpine lithosphere in great detail. The database is hereby openly shared to serve further research.
Martin Kobe, Gerald Gabriel, Adelheid Weise, and Detlef Vogel
Solid Earth, 10, 599–619,Short summary
Subrosion, i.e. the underground leaching of soluble rocks, causes disastrous sinkhole events worldwide. We investigate the accompanying mass transfer using quarter-yearly time-lapse gravity campaigns over 4 years in the town of Bad Frankenhausen, Germany. After correcting for seasonal soil water content, we find evidence of underground mass loss and attempt to quantify its amount. This is the first study of its kind to prove the feasibility of this approach in an urban area.
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: TectonicsConstruction of the Ukrainian Carpathian wedge from low-temperature thermochronology and tectono-stratigraphic analysisAnalogue modelling of basin inversion: a review and future perspectivesInsights into the interaction of a shale with CO2The influence of crustal strength on rift geometry and development – Insights from 3D numerical modellingTectonostratigraphic evolution of the Slyne BasinControl of crustal strength, tectonic inheritance, and stretching/ shortening rates on crustal deformation and basin reactivation: insights from laboratory modelsLate 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 GermanyEarthquake ruptures and topography of the Chilean margin controlled by plate interface deformationLate Quaternary faulting in the southern Matese (Italy): implications for earthquake potential and slip rate variability in the southern ApenninesRare earth elements associated with carbonatite–alkaline complexes in western Rajasthan, India: exploration targeting at regional scaleStructural complexities and tectonic barriers controlling recent seismic activity in the Pollino area (Calabria–Lucania, southern Italy) – constraints from stress inversion and 3D fault model buildingThe Mid Atlantic Appalachian Orogen Traverse: a comparison of virtual and on-location field-based capstone experiencesChronology 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 tomographyGround-penetrating radar signature of Quaternary faulting: a study from the Mt. Pollino region, southern Apennines, ItalyU–Pb dating of middle Eocene–Pliocene multiple tectonic pulses in the Alpine forelandDetrital 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 IraqThe Subhercynian Basin: an example of an intraplate foreland basin due to a broken plateHolocene surface-rupturing earthquakes on the Dinaric Fault System, western SloveniaContribution of gravity gliding in salt-bearing rift basins – a new experimental setup for simulating salt tectonics under the influence of sub-salt extension and tiltingThick- and thin-skinned basin inversion in the Danish Central Graben, North Sea – the role of deep evaporites and basement kinematicsComplex rift patterns, a result of interacting crustal and mantle weaknesses, or multiphase rifting? Insights from analogue modelsInteractions of plutons and detachments: a comparison of Aegean and Tyrrhenian granitoidsInsights from elastic thermobarometry into exhumation of high-pressure metamorphic rocks from Syros, GreeceStress rotation – impact and interaction of rock stiffness and faultsLate Cretaceous to Paleogene exhumation in central Europe – localized inversion vs. large-scale domal upliftKinematics and extent of the Piemont–Liguria Basin – implications for subduction processes in the AlpsEffects of basal drag on subduction dynamics from 2D numerical modelsHydrocarbon accumulation in basins with multiple phases of extension and inversion: examples from the Western Desert (Egypt) and the western Black SeaLong-wavelength late-Miocene thrusting in the north Alpine foreland: implications for late orogenic processesA reconstruction of Iberia accounting for Western Tethys–North Atlantic kinematics since the late-Permian–TriassicThe enigmatic curvature of Central Iberia and its puzzling kinematicsControl of 3-D tectonic inheritance on fold-and-thrust belts: insights from 3-D numerical models and application to the Helvetic nappe systemPlio-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 earthquakesSeismic reflection data reveal the 3D structure of the newly discovered Exmouth Dyke Swarm, offshore NW AustraliaCenozoic deformation in the Tauern Window (Eastern Alps) constrained by in situ Th-Pb dating of fissure monaziteUncertainties in break-up markers along the Iberia–Newfoundland margins illustrated by new seismic dataTectonic inheritance controls nappe detachment, transport and stacking in the Helvetic nappe system, Switzerland: insights from thermomechanical simulationsCan subduction initiation at a transform fault be spontaneous?The Geodynamic World Builder: a solution for complex initial conditions in numerical modelingFrom mapped faults to fault-length earthquake magnitude (FLEM): a test on Italy with methodological implicationsLithosphere tearing along STEP faults and synkinematic formation of lherzolite and wehrlite in the shallow subcontinental mantleA systematic comparison of experimental set-ups for modelling extensional tectonicsImproving subduction interface implementation in dynamic numerical modelsThe Bortoluzzi Mud Volcano (Ionian Sea, Italy) and its potential for tracking the seismic cycle of active faultsThe Ulakhan fault surface rupture and the seismicity of the Okhotsk–North America plate boundaryControl of increased sedimentation on orogenic fold-and-thrust belt structure – insights into the evolution of the Western AlpsAnticlockwise 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
Marion Roger, Arjan de Leeuw, Peter van der Beek, Laurent Husson, Edward R. Sobel, Johannes Glodny, and Matthias Bernet
Solid Earth, 14, 153–179,Short summary
We study the construction of the Ukrainian Carpathians with LT thermochronology (AFT, AHe, and ZHe) and stratigraphic analysis. QTQt thermal models are combined with burial diagrams to retrieve the timing and magnitude of sedimentary burial, tectonic burial, and subsequent exhumation of the wedge's nappes from 34 to ∼12 Ma. Out-of-sequence thrusting and sediment recycling during wedge building are also identified. This elucidates the evolution of a typical wedge in a roll-back subduction zone.
Frank Zwaan, Guido Schreurs, Susanne J. H. Buiter, Oriol Ferrer, Riccardo Reitano, Michael Rudolf, and Ernst Willingshofer
Solid Earth, 13, 1859–1905,Short summary
When a sedimentary basin is subjected to compressional tectonic forces after its formation, it may be inverted. A thorough understanding of such
basin inversionis of great importance for scientific, societal, and economic reasons, and analogue tectonic models form a key part of our efforts to study these processes. We review the advances in the field of basin inversion modelling, showing how the modelling results can be applied, and we identify promising venues for future research.
Eleni Stavropoulou and Lyesse Laloui
Solid Earth, 13, 1823–1841,Short summary
Shales are identified as suitable caprock formations for geolocigal CO2 storage thanks to their low permeability. Here, small-sized shale samples are studied under field-representative conditions with X-ray tomography. The geochemical impact of CO2 on calcite-rich zones is for the first time visualised, the role of pre-existing micro-fissures in the CO2 invasion trapping in the matererial is highlighted, and the initiation of micro-cracks when in contact with anhydrous CO2 is demonstrated.
Thomas Phillips, John Naliboff, Ken McCaffrey, Sophie Pan, Jeroen van Hunen, and Malte Froemchen
Continental crust comprises bodies of varying strength, formed through numerous tectonic events. When subject to extension these areas produce varying rift and fault systems. We use 3D models to examine how rifts form above ‘strong’ and ‘weak’ areas 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.
Conor M. O'Sullivan, Conrad J. Childs, Muhammad M. Saqab, John J. Walsh, and Patrick M. Shannon
Solid Earth, 13, 1649–1671,Short summary
The Slyne Basin is a sedimentary basin located offshore north-western Ireland. It formed through a long and complex evolution involving distinct periods of extension. The basin is subdivided into smaller basins, separated by deep structures related to the ancient Caledonian mountain-building event. These deep structures influence the shape of the basin as it evolves in a relatively unique way, where early faults follow these deep structures, but later faults do not.
Benjamin Guillaume, Guido M. Gianni, Jean-Jacques Kermarrec, and Khaled Bock
Solid Earth, 13, 1393–1414,Short summary
Under tectonic forces, the upper part of the crust can break along different types of faults, depending on the orientation of the applied stresses. Using scaled analogue models, we show that the relative magnitude of compressional and extensional forces as well as the presence of inherited structures resulting from previous stages of deformation control the location and type of faults. Our results gives insights into the tectonic evolution of areas showing complex patterns of deformation.
Andrzej Głuszyński and Paweł Aleksandrowski
Solid Earth, 13, 1219–1242,Short summary
Old seismic data recently reprocessed with modern software allowed us to study at depth the Late Cretaceous tectonic structures in the Permo-Mesozoic rock sequences in the Sudetes. The structures formed in response to Iberia collision with continental Europe. The NE–SW compression undulated the crystalline basement top and produced folds, faults and joints in the sedimentary cover. Our results are of importance for regional geology and in prospecting for deep thermal waters.
Luisa Röckel, Steffen Ahlers, Birgit Müller, Karsten Reiter, Oliver Heidbach, Andreas Henk, Tobias Hergert, and Frank Schilling
Solid Earth, 13, 1087–1105,Short summary
Reactivation of tectonic faults can lead to earthquakes and jeopardize underground operations. The reactivation potential is linked to fault properties and the tectonic stress field. We create 3D geometries for major faults in Germany and use stress data from a 3D geomechanical–numerical model to calculate their reactivation potential and compare it to seismic events. The reactivation potential in general is highest for NNE–SSW- and NW–SE-striking faults and strongly depends on the fault dip.
Nadaya Cubas, Philippe Agard, and Roxane Tissandier
Solid Earth, 13, 779–792,Short summary
Earthquake extent prediction is limited by our poor understanding of slip deficit patterns. From a mechanical analysis applied along the Chilean margin, we show that earthquakes are bounded by extensive plate interface deformation. This deformation promotes stress build-up, leading to earthquake nucleation; earthquakes then propagate along smoothed fault planes and are stopped by heterogeneously distributed deformation. Slip deficit patterns reflect the spatial distribution of this deformation.
Paolo Boncio, Eugenio Auciello, Vincenzo Amato, Pietro Aucelli, Paola Petrosino, Anna C. Tangari, and Brian R. Jicha
Solid Earth, 13, 553–582,Short summary
We studied the Gioia Sannitica normal fault (GF) within the southern Matese fault system (SMF) in southern Apennines (Italy). It is a fault with a long slip history that has experienced recent reactivation or acceleration. Present activity has resulted in late Quaternary fault scarps and Holocene surface faulting. The maximum slip rate is ~ 0.5 mm/yr. Activation of the 11.5 km GF or the entire 30 km SMF can produce up to M 6.2 or M 6.8 earthquakes, respectively.
Malcolm Aranha, Alok Porwal, Manikandan Sundaralingam, Ignacio González-Álvarez, Amber Markan, and Karunakar Rao
Solid Earth, 13, 497–518,Short summary
Rare earth elements (REEs) are considered critical mineral resources for future industrial growth due to their short supply and rising demand. This study applied an artificial-intelligence-based technique to target potential REE-deposit hosting areas in western Rajasthan, India. Uncertainties associated with the prospective targets were also estimated to aid decision-making. The presented workflow can be applied to similar regions elsewhere to locate potential zones of REE mineralisation.
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,Short summary
The Pollino region is a highly seismic area of Italy. Increasing the geological knowledge on areas like this contributes to reducing risk and saving lives. We reconstruct the 3D model of the faults which generated the 2010–2014 seismicity integrating geological and seismological data. Appropriate relationships based on the dimensions of the activated faults suggest that they did not fully discharge their seismic potential and could release further significant earthquakes in the near future.
Steven Whitmeyer, Lynn Fichter, Anita Marshall, and Hannah Liddle
Solid Earth, 12, 2803–2820,Short summary
Field trips in the Stratigraphy, Structure, Tectonics (SST) course transitioned to a virtual format in Fall 2020, due to the COVID pandemic. Virtual field experiences (VFEs) were developed in web Google Earth and were evaluated in comparison with on-location field trips via an online survey. Students recognized the value of VFEs for revisiting outcrops and noted improved accessibility for students with disabilities. Potential benefits of hybrid field experiences were also indicated.
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,Short summary
Molasse deposits, deposited and deformed at the western Alpine front during the Miocene (23 to 5.6 Ma), record the chronology of that deformation. We combine the first precise chronostratigraphy (precision of ∼0.5 Ma) of the Miocene molasse, the reappraisal of the regional structure, and the analysis of growth deformation structures in order to document three tectonic phases and the precise chronology of thrust westward propagation during the second one involving the Belledonne basal thrust.
Mark R. Handy, Stefan M. Schmid, Marcel Paffrath, Wolfgang Friederich, and the AlpArray Working Group
Solid Earth, 12, 2633–2669,Short summary
New images from the multi-national AlpArray experiment illuminate the Alps from below. They indicate thick European mantle descending beneath the Alps and forming blobs that are mostly detached from the Alps above. In contrast, the Adriatic mantle in the Alps is much thinner. This difference helps explain the rugged mountains and the abundance of subducted and exhumed units at the core of the Alps. The blobs are stretched remnants of old ocean and its margins that reach down to at least 410 km.
Maurizio Ercoli, Daniele Cirillo, Cristina Pauselli, Harry M. Jol, and Francesco Brozzetti
Solid Earth, 12, 2573–2596,Short summary
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,Short summary
In this paper, we dated fault movements at geological timescales which uplifted the sedimentary successions of the Jura Mountains from below the sea level up to Earth's surface. To do so, we applied the novel technique of U–Pb geochronology on calcite mineralizations that precipitated on fault surfaces during times of tectonic activity. Our results document a time frame of the tectonic evolution of the Jura Mountains and provide new insight into the broad geological history of the Western Alps.
Renas I. Koshnaw, Fritz Schlunegger, and Daniel F. Stockli
Solid Earth, 12, 2479–2501,Short summary
As continental plates collide, mountain belts grow. This study investigated the provenance of rocks from the northwestern segment of the Zagros mountain belt to unravel the convergence history of the Arabian and Eurasian plates. Provenance data synthesis and field relationships suggest that the Zagros Mountains developed as a result of the oceanic crust emplacement on the Arabian continental plate, followed by the Arabia–Eurasia collision and later uplift of the broader region.
David Hindle and Jonas Kley
Solid Earth, 12, 2425–2438,Short summary
Central western Europe underwent a strange episode of lithospheric deformation, resulting in a chain of small mountains that run almost west–east across the continent and that formed in the middle of a tectonic plate, not at its edges as is usually expected. Associated with these mountains, in particular the Harz in central Germany, are marine basins contemporaneous with the mountain growth. We explain how those basins came to be as a result of the mountains bending the adjacent plate.
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,Short summary
Several large strike-slip faults in western Slovenia are known to be active, but most of them have not produced strong earthquakes in historical times. In this study we use geomorphology, near-surface geophysics, and fault excavations to show that two of these faults had surface-rupturing earthquakes during the Holocene. Instrumental and historical seismicity data do not capture the strongest events in this area.
Michael Warsitzka, Prokop Závada, Fabian Jähne-Klingberg, and Piotr Krzywiec
Solid Earth, 12, 1987–2020,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.
Torsten Hundebøl Hansen, Ole Rønø Clausen, and Katrine Juul Andresen
Solid Earth, 12, 1719–1747,Short summary
We have analysed the role of deep salt layers during tectonic shortening of a group of sedimentary basins buried below the North Sea. Due to the ability of salt to flow over geological timescales, the salt layers are much weaker than the surrounding rocks during tectonic deformation. Therefore, complex structures formed mainly where salt was present in our study area. Our results align with findings from other basins and experiments, underlining the importance of salt tectonics.
Frank Zwaan, Pauline Chenin, Duncan Erratt, Gianreto Manatschal, and Guido Schreurs
Solid Earth, 12, 1473–1495,Short summary
We used laboratory experiments to simulate the early evolution of rift systems, and the influence of structural weaknesses left over from previous tectonic events that can localize new deformation. We find that the orientation and type of such weaknesses can induce complex structures with different orientations during a single phase of rifting, instead of requiring multiple rifting phases. These findings provide a strong incentive to reassess the tectonic history of various natural examples.
Laurent Jolivet, Laurent Arbaret, Laetitia Le Pourhiet, Florent Cheval-Garabédian, Vincent Roche, Aurélien Rabillard, and Loïc Labrousse
Solid Earth, 12, 1357–1388,Short summary
Although viscosity of the crust largely exceeds that of magmas, we show, based on the Aegean and Tyrrhenian Miocene syn-kinematic plutons, how the intrusion of granites in extensional contexts is controlled by crustal deformation, from magmatic stage to cold mylonites. We show that a simple numerical setup with partial melting in the lower crust in an extensional context leads to the formation of metamorphic core complexes and low-angle detachments reproducing the observed evolution of plutons.
Miguel Cisneros, Jaime D. Barnes, Whitney M. Behr, Alissa J. Kotowski, Daniel F. Stockli, and Konstantinos Soukis
Solid Earth, 12, 1335–1355,Short summary
Constraining the conditions at which rocks form is crucial for understanding geologic processes. For years, the conditions under which rocks from Syros, Greece, formed have remained enigmatic; yet these rocks are fundamental for understanding processes occurring at the interface between colliding tectonic plates (subduction zones). Here, we constrain conditions under which these rocks formed and show they were transported to the surface adjacent to the down-going (subducting) tectonic plate.
Solid Earth, 12, 1287–1307,Short summary
The influence and interaction of elastic material properties (Young's modulus, Poisson's ratio), density and low-friction faults on the resulting far-field stress pattern in the Earth's crust is tested with generic models. A Young's modulus contrast can lead to a significant stress rotation. Discontinuities with low friction in homogeneous models change the stress pattern only slightly, away from the fault. In addition, active discontinuities are able to compensate stress rotation.
Hilmar von Eynatten, Jonas Kley, István Dunkl, Veit-Enno Hoffmann, and Annemarie Simon
Solid Earth, 12, 935–958,
Eline Le Breton, Sascha Brune, Kamil Ustaszewski, Sabin Zahirovic, Maria Seton, and R. Dietmar Müller
Solid Earth, 12, 885–913,Short summary
The former Piemont–Liguria Ocean, which separated Europe from Africa–Adria in the Jurassic, opened as an arm of the central Atlantic. Using plate reconstructions and geodynamic modeling, we show that the ocean reached only 250 km width between Europe and Adria. Moreover, at least 65 % of the lithosphere subducted into the mantle and/or incorporated into the Alps during convergence in Cretaceous and Cenozoic times comprised highly thinned continental crust, while only 35 % was truly oceanic.
Lior Suchoy, Saskia Goes, Benjamin Maunder, Fanny Garel, and Rhodri Davies
Solid Earth, 12, 79–93,Short summary
We use 2D numerical models to highlight the role of basal drag in subduction force balance. We show that basal drag can significantly affect velocities and evolution in our simulations and suggest an explanation as to why there are no trends in plate velocities with age in the Cenozoic subduction record (which we extracted from recent reconstruction using GPlates). The insights into the role of basal drag will help set up global models of plate dynamics or specific regional subduction models.
William Bosworth and Gábor Tari
Solid Earth, 12, 59–77,Short summary
Many of the world's hydrocarbon resources are found in rifted sedimentary basins. Some rifts experience multiple phases of extension and inversion. This results in complicated oil and gas generation, migration, and entrapment histories. We present examples of basins in the Western Desert of Egypt and the western Black Sea that were inverted multiple times, sometimes separated by additional phases of extension. We then discuss how these complex deformation histories impact exploration campaigns.
Samuel Mock, Christoph von Hagke, Fritz Schlunegger, István Dunkl, and Marco Herwegh
Solid Earth, 11, 1823–1847,Short summary
Based on thermochronological data, we infer thrusting along-strike the northern rim of the Central Alps between 12–4 Ma. While the lithology influences the pattern of thrusting at the local scale, we observe that thrusting in the foreland is a long-wavelength feature occurring between Lake Geneva and Salzburg. This coincides with the geometry and dynamics of the attached lithospheric slab at depth. Thus, thrusting in the foreland is at least partly linked to changes in slab dynamics.
Paul Angrand, Frédéric Mouthereau, Emmanuel Masini, and Riccardo Asti
Solid Earth, 11, 1313–1332,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.
Daniel Pastor-Galán, Gabriel Gutiérrez-Alonso, and Arlo B. Weil
Solid Earth, 11, 1247–1273,Short summary
Pangea was assembled during Devonian to early Permian times and resulted in a large-scale and winding orogeny that today transects Europe, northwestern Africa, and eastern North America. This orogen is characterized by an
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,Short summary
We apply three-dimensional (3D) thermo-mechanical numerical simulations of the shortening of the upper crustal region of a passive margin in order to investigate the control of 3D laterally variable inherited structures on fold-and-thrust belt evolution and associated nappe formation. The model is applied to the Helvetic nappe system of the Swiss Alps. Our results show a 3D reconstruction of the first-order tectonic evolution showing the fundamental importance of inherited geological structures.
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,Short summary
The Alboran Sea is one of the most active region of the Mediterranean Sea. There, the basin architecture records the effect of the Africa–Eurasia plates convergence. We evidence a Pliocene transpression and a more recent Pleistocene tectonic reorganization. We propose that main driving force of the deformation is the Africa–Eurasia convergence, rather than other geodynamical processes. It highlights the evolution and the geometry of the present-day Africa–Eurasia plate boundary.
Dan J. Clark, Sarah Brennand, Gregory Brenn, Matthew C. Garthwaite, Jesse Dimech, Trevor I. Allen, and Sean Standen
Solid Earth, 11, 691–717,Short summary
A magnitude 5.3 reverse-faulting earthquake in September 2018 near Lake Muir in southwest Western Australia was followed after 2 months by a collocated magnitude 5.2 strike-slip event. The first event produced a ~ 5 km long and up to 0.5 m high west-facing surface rupture, and the second triggered event deformed but did not rupture the surface. The earthquake sequence was the ninth to have produced surface rupture in Australia. None of these show evidence for prior Quaternary surface rupture.
Craig Magee and Christopher Aiden-Lee Jackson
Solid Earth, 11, 579–606,Short summary
Injection of vertical sheets of magma (dyke swarms) controls tectonic and volcanic processes on Earth and other planets. Yet we know little of the 3D structure of dyke swarms. We use seismic reflection data, which provides ultrasound-like images of Earth's subsurface, to study a dyke swarm in 3D for the first time. We show that (1) dyke injection occurred in the Late Jurassic, (2) our data support previous models of dyke shape, and (3) seismic data provides a new way to view and study dykes.
Emmanuelle Ricchi, Christian A. Bergemann, Edwin Gnos, Alfons Berger, Daniela Rubatto, Martin J. Whitehouse, and Franz Walter
Solid Earth, 11, 437–467,Short summary
This study investigates Cenozoic deformation during cooling and exhumation of the Tauern metamorphic and structural dome, Eastern Alps, through Th–Pb dating of fissure monazite-(Ce). Fissure (or hydrothermal) monazite-(Ce) typically crystallizes in a temperature range of 400–200 °C. Three major episodes of monazite growth occurred at approximately 21, 17, and 12 Ma, corroborating previous crystallization and cooling ages.
Annabel Causer, Lucía Pérez-Díaz, Jürgen Adam, and Graeme Eagles
Solid Earth, 11, 397–417,Short summary
Here we discuss the validity of so-called “break-up” markers along the Newfoundland margin, challenging their perceived suitability for plate kinematic reconstructions of the southern North Atlantic. We do this on the basis of newly available seismic transects across the Southern Newfoundland Basin. Our new data contradicts current interpretations of the extent of oceanic lithosphere and illustrates the need for a differently constraining the plate kinematics of the Iberian plate pre M0 times.
Dániel Kiss, Thibault Duretz, and Stefan Markus Schmalholz
Solid Earth, 11, 287–305,Short summary
In this paper, we investigate the physical mechanisms of tectonic nappe formation by high-resolution numerical modeling. Tectonic nappes are key structural features of many mountain chains which are packets of rocks displaced, sometimes even up to 100 km, from their original position. However, the physical mechanisms involved are not fully understood. We solve numerical equations of fluid and solid dynamics to improve our knowledge. The results are compared with data from the Helvetic Alps.
Diane Arcay, Serge Lallemand, Sarah Abecassis, and Fanny Garel
Solid Earth, 11, 37–62,Short summary
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,Short summary
Three-dimensional numerical modelling of geodynamic processes may benefit strongly from using realistic 3-D starting models that approximate, e.g. natural subduction settings in the geological past or at present. To this end, we developed the Geodynamic World Builder (GWB), which enables relatively straightforward parameterization of complex 3-D geometric structures associated with geodynamic processes. The GWB is an open-source community code designed to easily interface with geodynamic codes.
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,Short summary
Considering all mapped faults in Italy, empirical scaling laws between fault dimensions and earthquake magnitude are used at the national scale. Results are compared with earthquake catalogues. The consistency between our results and the catalogues gives credibility to the method. Some large differences between the two datasets suggest the validation of this experiment elsewhere.
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,Short summary
Subduction-transform edge propagator (STEP) faults are the locus of continual lithospheric tearing at the edges of subducted slabs, resulting in sharp changes in the lithospheric thickness and triggering lateral and/or near-vertical mantle flow. Here, we study upper mantle rocks recovered from a STEP fault context by < 4 Ma alkali volcanism. We reconstruct how the microstructure developed during deformation and coupled melt–rock interaction, which are promoted by lithospheric tearing at depth.
Frank Zwaan, Guido Schreurs, and Susanne J. H. Buiter
Solid Earth, 10, 1063–1097,Short summary
This work was inspired by an effort to numerically reproduce laboratory models of extension tectonics. We tested various set-ups to find a suitable analogue model and in the process systematically charted the impact of set-ups and boundary conditions on model results, a topic poorly described in existing scientific literature. We hope that our model results and the discussion on which specific tectonic settings they could represent may serve as a guide for future (analogue) modeling studies.
Dan Sandiford and Louis Moresi
Solid Earth, 10, 969–985,Short summary
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,Short summary
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,Short summary
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,Short summary
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,Short summary
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.
Asch, K.: IGME 5000: 1:5 Million International Geological Map of Europe and Adjacent Areas, Bundesanstalt für Geowissenschaften und Rohstoffe, Hannover, 2005.
Barrier, E., Chamot-Rooke, N., and Giordano, G.: Geodynamic map of the Mediterranean, 2004.
Bauberger, W. and Cramer, P. (Eds.): Erl. Geol. Kt. Bayern 1:25.000, Bl. 6838 Regenstauf, München, 220 pp., 1961.
Beer, W. W.: Die strukturelle Entwicklung der Metamorphite des Bayerischen Waldes, PhD thesis, Mathematisch-Naturwissenschaftliche Fakultät, Georg-August-Universität Göttingen, Göttingen, 186 pp., 1981.
Behr, H.-J., Große, S., Heinrichs, T., and Wolf, U.: A Reinterpretation of the Gravity Field in the Surroundings of the KTB Drill Site – Implications for Granite Plutonism and Terrane Tectonics in the Variscan, in: The German continental deep drilling program (KTB): Site selection studies in the Oberpfalz and Schwarzwald, edited by: Emmermann, R. and Wohlenberg, J., Springer, Berlin, Heidelberg, New York, London, Paris, Tokyo, Hong Kong, 501–525, 1989.
Blümel, P.: Die Analyse von Kristallisation und Deformation einer metamorphen Zonenfolge im Moldanubikum von Lam-Bodenmais, E-Bayern, N. Jb. Miner. Abh., 118, 74–96, 1972.
Blümel, P. and Schreyer, W.: Phase Relations in Pelitic and Psammitic Gneisses of the Sillimanite-Potash Feldspar and Cordierite-Potash Feldspar Zones in the Moldanubicum of the Lam-Bodenmais Area, Bavaria, J. Petrol., 18, 431–459, https://doi.org/10.1093/petrology/18.3.431, 1977.
Blümel, P. and Schreyer, W.: Progressive regional low-pressure metamorphism in Moldanubian metapelites of the northern Bavarian Forest, Germany, Krystallinikum, 12, 7–30, 1976.
Brandmayr, M., Dallmeyer, R. D., Handler, R., and Wallbrecher, E.: Conjugate shear zones in the Southern Bohemian Massif (Austria): implications for Variscan and Alpine tectonothermal activity, Tectonophysics, 248, 97–116, https://doi.org/10.1016/0040-1951(95)00003-6, 1995.
Brown, M.: The definition of metatexis, diatexis and migmatite, Proc. Geol. Ass., 84, 371–382, https://doi.org/10.1016/S0016-7878(73)80021-5, 1973.
Burbank, D. W. and Anderson, R. S.: Tectonic geomorphology, 2nd ed., J. Wiley & Sons, Chichester, West Sussex, Hoboken, N.J, 454 pp., 2012.
Butler, R. W. H., Harris, N. B. W., and Whittington, A. G.: Interactions between deformation, magmatism and hydrothermal activity during active crustal thickening: a field example from Nanga Parbat, Pakistan Himalayas, Mineral. Mag., 61, 37–52, https://doi.org/10.1180/minmag.1997.061.404.05, 1997.
Büttner, S. H.: Late Variscan stress-field rotation initiating escape tectonics in the south-western Bohemian Massif: a far field response to late-orogenic extension, J. Geosci., 52, 29–43, https://doi.org/10.3190/jgeosci.004, 2007.
Büttner, S. H.: The geometric evolution of structures in granite during continuous deformation from magmatic to solid-state conditions: an example from the central European Variscan Belt, American Mineral., 84, 1781–1792, https://doi.org/10.2138/am-1999-11-1207, 1999.
Carlé, W.: Bau und Entwicklung der Südwestdeutschen Großscholle, Beihefte zum Geologischen Jahrbuch, 16, Schweizerbart Science Publishers, Stuttgart, 272 pp., 1955.
Chen, F. and Siebel, W.: Zircon and titanite geochronology of the Fürstenstein granite massif, Bavarian Forest, NW Bohemian Massif: Pulses of the late Variscan magmatic activity, Eur. J. Mineral., 16, 777–788, https://doi.org/10.1127/0935-1221/2004/0016-0777, 2004.
Chen, F., Siebel, W., and Satir, M.: Geochemical and isotopic composition and inherited zircon ages as evidence for lower crustal origin of two Variscan S-type granites in the NW Bohemian Massif, Int. J. Earth Sci. (Geol. Rundsch.), 92, 173–184, https://doi.org/10.1007/s00531-003-0310-6, 2003.
Chen, G.-N. and Grapes, R.: Granite Genesis: In-Situ Melting and Crustal Evolution, Springer Science + Business Media B.V, Dordrecht, 278 pp., 2007.
Crameri, F.: Scientific colour maps, Zenodo, https://doi.org/10.5281/zenodo.1243862, 2021.
Crameri, F., Shephard, G. E., and Heron, P. J.: The misuse of colour in science communication, Nat. Commun., 11, 5444, https://doi.org/10.1038/s41467-020-19160-7, 2020.
Cymerman, Z., Piasecki, M. A. J., and Seston, R.: Terranes and terrane boundaries in the Sudetes, northeast Bohemian Massif, Geol. Mag., 134, 717–725, https://doi.org/10.1017/S0016756897007255, 1997.
Daurer, A.: Das Moldanubikum im Bereich der Donaustörung zwischen Jochenstein und Schlögen (Oberösterreich), Mitt. Ges. Geol. Bergbaustud. Österr., 23, 1–54, 1976.
Davis, J. C.: Statistics and data analysis in geology, 3rd ed., Wiley, New York, 638 pp., 2002.
de Wall, H., Schaarschmidt, A., Kämmlein, M., Gabriel, G., Bestmann, M., and Scharfenberg, L.: Subsurface granites in the Franconian Basin as the source of enhanced geothermal gradients: a key study from gravity and thermal modeling of the Bayreuth Granite, Int. J. Earth Sci. (Geol. Rundsch.), 108, 1913–1936, https://doi.org/10.1007/s00531-019-01740-8, 2019.
Dietl, C., Gößmann, M., and de Wall, H.: Kombinierte aktive und passive Plutonplatznahme in einer verdickten Kruste - Erste Ergebnisse von gesteinsmagnetischen und petrologischen Untersuchungen am Fürstensteiner lntrusivkomplex (Bayerischer Wald), Z. dt. geol. Ges., 155, 311–328, 2005.
Drury, S. A.: Image interpretation in geology, 2. ed., Chapman & Hall, London, 283 pp., 1987.
Earth Resources Observation And Science Center: Shuttle Radar Topography Mission (SRTM) 1 Arc-Second Global [data set], https://doi.org/10.5066/F7PR7TFT, 2017.
Echtler, H. P. and Chauvet, A.: Carboniferous convergence and subsequent crustal extension in the southern Schwarzwald (SW Germany), Geodin. Acta, 5, 37–49, https://doi.org/10.1080/09853111.1992.11105218, 1992.
Fatka, O. and Mergl, M.: The “microcontinent” Perunica: status and story 15 years after conception, Geol. Soc. Spec. Publ., 325, 65–101, https://doi.org/10.1144/SP325.4, 2009.
Finger, F. and René, M.: A Comment on “Two Distinctive Granite Suites in the SW Bohemian Massif and their Record of Emplacement: Constraints from Geochemistry and Zircon 207Pb/206Pb Chronology” by Siebel et al., Journal of Petrology 49, 1853-1872, J. Petrol, 50, 591–593, https://doi.org/10.1093/petrology/egp013, 2009.
Finger, F. and Clemens, J. D.: Migmatization and “secondary” granitic magmas: effects of emplacement and crystallization of “primary” granitoids in Southern Bohemia, Austria, Contrib. Mineral. and Petrol., 120, 311–326, https://doi.org/10.1007/BF00306510, 1995.
Finger, F., Dunkley, D. J., and René, M.: Remnants of Early Carboniferous I-type granodiorite plutons in the Bavarian Forest and their bearing on the tectonic interpretation of the south-western sector of the Bohemian Massif (Bavarian Zone), J. Geosci., 55, 321–332, https://doi.org/10.3190/jgeosci.080, 2010.
Finger, F., Gerdes, A., Janoušek, V., René, M., and Riegler, G.: Resolving the Variscan evolution of the Moldanubian sector of the Bohemian Massif: the significance of the Bavarian and the Moravo-Moldanubian tectonometamorphic phases, J. Geosci., 52, 9–28, https://doi.org/10.3190/jgeosci.005, 2007.
Franke, W.: The mid-European segment of the Variscides: tectonostratigraphic units, terrane boundaries and plate tectonic evolution, Geol. Soc. Spec. Publ., 179, 35–61, https://doi.org/10.1144/GSL.SP.2000.179.01.05, 2000.
Franke, W.: Tectonostratigraphic units in the Variscan belt of central Europe, in: Terranes in the Circum-Atlantic Paleozoic Orogens, edited by: Dallmeyer, R. D., Geological Society of America, Boulder, Colo., 67–90, https://doi.org/10.1130/SPE230-p67, 1989.
Freudenberger, W.: Tektonik, in: Erläuterungen zur Geologischen Karte von Bayern 1:500 000, 4th ed., edited by: Bayerisches Geologisches Landesamt, München, 259–265, 1996.
Freudenberger, W. and Schwerd, K.: Tektonische Karte von Bayern 1:1000000, in: Erläuterungen zur Geologischen Karte von Bayern 1:500 000, 4th ed., edited by: Bayerisches Geologisches Landesamt, München, 1996.
Führer, F. X.: Die Anomalien der Schwere am Südwest-Rand des Bayerischen Waldes und ihre Interpretation, Int. J. Earth Sci. (Geol. Rundsch.), 67, 1078–1096, https://doi.org/10.1007/BF01983255, 1978.
Fürst, M., Krupp, R., and Müller, R.: Die photogeologische Linearanalyse und ihre Anwendung bei der Uranprospektion in der Oberpfalz, Erlanger geol. Abh., 3–33, 1978.
Galadí-Enríquez, E., Dörr, W., Zulauf, G., Galindo-Zaldívar, J., Heidelbach, F., and Rohrmüller, J.: Variscan deformation phases in the southwestern Bohemian Massif: new constraints from sheared granitoids, Z. dt. Ges. Geowiss., 161, 1–23, https://doi.org/10.1127/1860-1804/2010/0161-0001, 2010.
Galadí-Enríquez, E., Kroemer, E., Loth, G., Pürner, T., Raum, G., Teipel, U., and Rohrmüller, J.: Erdgeschichte des Oberpfälzer Waldes: Geologischer Bau, Gesteine, Sehenswürdigkeiten, Erläuterungen zur Geologischen Karte des Oberpfälzer Waldes, Augsburg, 110 pp., 2009a.
Galadí-Enríquez, E., Kroemer, E., Loth, G., Pürner, T., Raum, G., Teipel, U., and Rohrmüller, J.: Geologische Karte des Oberpfälzer Waldes 1:150000, Bayerisches Landesamt für Umwelt, Augsburg, 2009b.
Gebauer, D.: Erdgeschichtliche Entwicklung und geologischer Überblick, in: Erl. Geol. Kt. Bayern 1:25.000, Bl. 7446 Passau, edited by: Bauberger, W. and Unger, H. J., München, 13–22, 1984.
Gerdes, A., Finger, F., and Parrish, R. R.: Southwestward progression of a late-orogenic heat front in the Moldanubian Zone of the Bohemian Massif and formation of the Austro-Bavarian anatexite belt, Geophys. Res. Abstr., 8, SRef-ID: 1607-7962/gra/EGU06-A-10698, 2006.
Goldsworthy, M. and Jackson, J.: Active normal fault evolution in Greece revealed by geomorphology and drainage patterns, J. Geol. Soc., 157, 967–981, https://doi.org/10.1144/jgs.157.5.967, 2000.
Grauert, B., Hänny, R., and Soptrajanova, G.: Geochronology of a Polymetamorphic and Anatectic Gneiss Region: The Moldanubicum of the Area Lam-Deggendorf, Eastern Bavaria, Germany, Contrib. Mineral. Petrol., 45, 37–63, https://doi.org/10.1007/BF00371136, 1974.
Guy, A., Edel, J.-B., Schulmann, K., Tomek, Č., and Lexa, O.: A geophysical model of the Variscan orogenic root (Bohemian Massif): Implications for modern collisional orogens, Lithos, 124, 144–157, https://doi.org/10.1016/j.lithos.2010.08.008, 2011.
Healy, D., Rizzo, R. E., Cornwell, D. G., Farrell, N. J., Watkins, H., Timms, N. E., Gomez-Rivas, E., and Smith, M.: FracPaQ: A MATLAB™ toolbox for the quantification of fracture patterns, J. Struct. Geol., 95, 1–16, https://doi.org/10.1016/j.jsg.2016.12.003, 2017.
Hejl, E., Coyle, D., Nand Lal, Van den Haute, P., and Wagner, G. A.: Fission-track dating of the western border of the Bohemian Massif: thermochronology and tectonic implications, Int. J. Earth Sci. (Geol. Rundsch.), 86, 210–219, https://doi.org/10.1007/s005310050133, 1997.
Horn, P., Köhler, H., and Müller-Sohnius, D.: Rb-Sr-Isotopengeochemie hydrothermaler Quarze des Bayerischen Pfahles und eines Flusspat-Schwerspatganges von Nabburg-Wölsendorf/Bundesrepublik Deutschland, Chem. Geol. Isot. Geosci. Sect., 58, 259–272, https://doi.org/10.1016/0168-9622(86)90015-1, 1986.
Jordan, G., Meijninger, B. M. L., van Hinsbergen, D. J. J., Meulenkamp, J. E., and van Dijk, P. M.: Extraction of morphotectonic features from DEMs: Development and applications for study areas in Hungary and NW Greece, Int. J. Appl. Earth Obs. Geoinf., 7, 163–182, https://doi.org/10.1016/j.jag.2005.03.003, 2005.
Kalt, A., Berger, A., and Blümel, P.: Metamorphic Evolution of Cordierite-Bearing Migmatites from the Bayerische Wald (Variscan Belt, Germany), J. Petrol, 40, 601–627, https://doi.org/10.1093/petroj/40.4.601, 1999.
Kalt, A., Corfu, F., and Wijbrans, J. R.: Time calibration of a P-T path from a Variscan high-temperature low-pressure metamorphic complex (Bayerische Wald, Germany), and the detection of inherited monazite, Contrib. Mineral. and Petrol., 138, 143–163, https://doi.org/10.1007/s004100050014, 2000.
Keller, E. A. and Pinter, N.: Active tectonics: Earthquakes, uplift, and landscape, 2nd ed., Prentice Hall earth science series, Prentice Hall, Upper Saddle River NJ, XIII, 362 S, 2002.
Klein, T., Kiehm, S., Siebel, W., Shang, C. K., Rohrmüller, J., Dörr, W., and Zulauf, G.: Age and emplacement of late-Variscan granites of the western Bohemian Massif with main focus on the Hauzenberg granitoids (European Variscides, Germany), Lithos, 102, 478–507, https://doi.org/10.1016/j.lithos.2007.07.025, 2008.
Kley, J. and Voigt, T.: Late Cretaceous intraplate thrusting in central Europe: Effect of Africa-Iberia-Europe convergence, not Alpine collision, Geology, 36, 839–842, https://doi.org/10.1130/G24930A.1, 2008.
Klomínský, J., Jarchovský, T., and Rajpoot, G. S.: ATLAS of plutonic rocks and orthogneisses in the Bohemian Massif: MOLDANUBICUM, Czech Geological Survey, Prague, 199 pp., 2010.
Kossmat, F.: Gliederung des varistischen Gebirgebaus, Abhandlungen des Sächsischen Geologischen Landesamts, 1, 1–39, 1927.
Krohe, A.: Variscan tectonics of central Europe: Postaccretionary intraplate deformation of weak continental lithosphere, Tectonics, 15, 1364–1388, https://doi.org/10.1029/96TC01110, 1996.
Kroner, U. and Romer, R. L.: Two plates – Many subduction zones: The Variscan orogeny reconsidered, Gondwana Research, 24, 298–329, https://doi.org/10.1016/j.gr.2013.03.001, 2013.
Kroner, U., Mansy, J.-L., Mazur, S., Aleksandrowski, P., Hann, H. P., Huckriede, H., Lacquement, F., Lamarche, J., Ledru, P., Pharaoh, T. C., Zedler, H., Zeh, A., and Zulauf, G.: Variscan Tectonics, in: The geology of Central Europe: Volume 1: Precambrian and Palaeozoic, edited by: McCann, T., The Geological Society London, London, 599–664, 2008.
Lehrberger, G., Saurle, A., and Hartmann, U.: Anwendung des SAR-DGM bei der tektonischen Interpretation des Moldanubikums am Westrand der Böhmischen Masse, in: Geologica Bavarica Nr. 107: Zur Geologie der Nordostbayerischen Grundgebirgsregion, edited by: Bayerisches Geologisches Landesamt, München, 269–280, 2003.
Leibniz-Institut für Angewandte Geophysik: Schwerekarte der Bundesrepublik Deutschland 1:1 000 000, Bouguer Anomalien, LIAG, Hannover, 2010.
Linnemann, U., McNaughton, N. J., Romer, R. L., Gehmlich, M., Drost, K., and Tonk, C.: West African provenance for Saxo-Thuringia (Bohemian Massif): Did Armorica ever leave pre-Pangean Gondwana? – U/Pb-SHRIMP zircon evidence and the Nd-isotopic record, Int. J. Earth Sci. (Geol. Rundsch.), 93, 683–705, https://doi.org/10.1007/s00531-004-0413-8, 2004.
Lowrie, W.: Fundamentals of Geophysics, 2. ed., 4th printing, Cambridge Univ. Press, Cambridge, 381 pp., 2007.
Matte, P.: Tectonics and plate tectonics model for the Variscan belt of Europe, Tectonophysics, 126, 329–374, https://doi.org/10.1016/0040-1951(86)90237-4, 1986.
Mattern, F.: Late Carboniferous to early Triassic shear sense reversals at strike-slip faults in eastern Bavaria, Zbl. Geol. Paläontol. Teil I, 1993, 1471–1490, 1995.
Meyer, R. K. F.: Tektonik des Deckgebirges, in: Erl. Geol. Kt. Bayern 1:25.000, Bl. 6639 Wackersdorf, edited by: Meyer, R. K. F. and Mielke, H., 118–121, 1993.
Meyer, R. K. F.: Die Entwicklung der Pfahl-Störungszone und des Bodenwöhrer Halbgrabens auf Blatt Wackersdorf, Erlanger geol. Abh., 117, 1–24, 1989.
Mielke, H.: Geologische Entwicklung des Kristallins, in: Erl. Geol. Kt. Bayern 1:25.000, Bl. 6639 Wackersdorf, edited by: Meyer, R. K. F. and Mielke, H., 10–12, 1993.
Müller, M.: Neue Vorstellungen zur Entwicklung des Nordostbayerischen Permokarbon-Trogs aufgrund reflexionsseismischer Messungen in der Mittleren Oberpfalz, Geol. Bl. NO-Bayern, 44, 195–224, 1994.
Neubauer, F. and Handler, R.: Variscan orogeny in the Eastern Alps and Bohemian Massif: How do these units correlate?, Mitt. Österr. Geol. Ges., 92, 35–59, 2000.
Pérez-Peña, J. V., Al-Awabdeh, M., Azañón, J. M., Galve, J. P., Booth-Rea, G., and Notti, D.: SwathProfiler and NProfiler: Two new ArcGIS Add-ins for the automatic extraction of swath and normalized river profiles, Comput. Geosci., 104, 135–150, https://doi.org/10.1016/j.cageo.2016.08.008, 2017.
Peterek, A., Rauche, H., Schröder, B., Franzke, H.-J., Bankwitz, P., and Bankwitz, E.: The late- and post-Variscan tectonic evolution of the Western Border fault zone of the Bohemian Massif (WBZ), Int. J. Earth Sci. (Geol. Rundsch.), 86, 191–202, https://doi.org/10.1007/s005310050131, 1997.
Peterek, A., Schröder, B., and Menzel, D.: Zur postvariszischen Krustenentwicklung des Naabgebirges und seines Rahmens, Z. geol. Wiss., 24, 293–304, 1996.
Priehäusser, G.: Felsfreistellungen, Blockmeere, Blockströme und Blockstreuungen im Bayer. Wald, Geol. Bl. NO-Bayern, 11, 123–132, 1961.
Propach, G., Kling, M., Linhardt, E., and Rohrmüller, J.: Remnants of an island arc within the Moldanubian zone of the Bavarian Forest, in: Geologica Bavarica Nr. 110: Geochronologische, geochemische, petrographische und mineralogische Untersuchungen im Grundgebirge Bayerns sowie kritische Betrachtungen zu Sr-Isotopenstandards, edited by: Bayerisches Landesamt für Umwelt, Augsburg, 343–377, 2008.
Propach, G., Baumann, A., Schulz-Schmalschläger, M., and Grauert, B.: Zircon and monazite U-Pb ages of Variscan granitoid rocks and gneisses in the Moldanubian zone of eastern Bavaria, Germany, N. Jb. Geol. Paläont. Mh., 2000, 345–377, https://doi.org/10.1127/njgpm/2000/2000/345, 2000.
Prost, G. L.: Remote Sensing for Geologists: A Guide to Image Interpretation, Gordon and Breach Science Publichers, Amsterdam, 326 pp., 1994.
Read, H. H.: Metamorphism and migmatisation in the Ythan Valley, Aberdeenshire, Transactions of the Edinburgh Geological Society, 15, 265–279, https://doi.org/10.1144/transed.15.1.265, 1952.
Rohrmüller, J., Artmann, C., and Teipel, U.: Das kristalline Grundgebirge des Moldanubikums von der Donau bis zur Pfahlzone (Exkursion L am 21. April 2017): The crystalline basement of the Moldanubian from the Danube to the Bavarian Pfahl Zone, Jber. Mitt. oberrhein. geol. Ver., 99, 345–370, https://doi.org/10.1127/jmogv/99/0011, 2017.
Rohrmüller, J., Mielke, H., and Gebauer, D.: Gesteinsfolge des Grundgebirges nördlich der Donau und im Molasseuntergrund, in: Erläuterungen zur Geologischen Karte von Bayern 1:500 000, 4th ed., edited by: Bayerisches Geologisches Landesamt, München, 16–54, 1996.
Rosenberg, C. L.: Shear zones and magma ascent: A model based on a review of the Tertiary magmatism in the Alps, Tectonics, 23, https://doi.org/10.1029/2003TC001526, 2004.
Schaarschmidt, A., Haase, K. M., de Wall, H., Bestmann, M., Krumm, S., and Regelous, M.: Upper crustal fluids in a large fault system: microstructural, trace element and oxygen isotope study on multi-phase vein quartz at the Bavarian Pfahl, SE Germany, Int. J. Earth Sci. (Geol. Rundsch.), 108, 521–543, https://doi.org/10.1007/s00531-018-1666-y, 2019.
Scheiber, T., Fredin, O., Viola, G., Jarna, A., Gasser, D., and Łapińska-Viola, R.: Manual extraction of bedrock lineaments from high-resolution LiDAR data: methodological bias and human perception, GFF, 137, 362–372, https://doi.org/10.1080/11035897.2015.1085434, 2015.
Schreyer, W. and Blümel, P.: Progressive metamorphism in the Moldanubicum of the Northern Bavarian Forest, Fortschritte der Mineralogie, 52, 151–165, 1974.
Schreyer, W., Kullerud, G., and Ramdohr, P.: Metamorphic conditions of ore and country rock of the Bodenmais, Bavaria, sulfide deposit, N. Jb. Miner. Abh., 101, 1–26, 1964.
Schröder, B.: Outline of the Permo-Carboniferous basins at the western margin of the Bohemian Massif, Z. geol. Wiss., 16, 993–1001, 1988.
Schröder, B., Ahrendt, H., Peterek, A., and Wemmer, K.: Post-Variscan sedimentary record of the SW margin of the Bohemian Massif: a review, Int. J. Earth Sci. (Geol. Rundsch.), 86, 178–184, https://doi.org/10.1007/s005310050129, 1997.
Schulmann, K., Catalán, J. R. M., Lardeaux, J. M., Janoušek, V., and Oggiano, G.: The Variscan orogeny: extent, timescale and the formation of the European crust, Geol. Soc. Spec. Publ., 405, 1–6, https://doi.org/10.1144/SP405.15, 2014.
Sedlák, J., Gnojek, I., Scheibe, R., and Zabadal, S.: Gravity response of igneous rocks in the northwestern part of the Bohemian Massif, J. Geosci., 54, 325–342, https://doi.org/10.3190/jgeosci.054, 2009.
Sedlák, J., Gnojek, I., Zabadal, S., Farbisz, J., Cwojdzinski, S., and Scheibe, R.: Geological interpretation of a gravity low in the central part of the Lugian Unit (Czech Republic, Germany and Poland), J. Geosci., 52, 181–197, https://doi.org/10.3190/jgeosci.012, 2007.
Seemann, R.: Die geologischen Verhältnisse längs der Amberg-Sulzbacher und Auerbach-Pegnitzer Störung: Beitrag zur Entstehung der Amberger Erzlager, Abh. naturhist. Ges. Nürnberg, 22, 93–149, 1925.
Siebel, W., Shang, C. K., Thern, E., Danišík, M., and Rohrmüller, J.: Zircon response to high-grade metamorphism as revealed by U–Pb and cathodoluminescence studies, Int. J. Earth Sci. (Geol. Rundsch.), 101, 2105–2123, https://doi.org/10.1007/s00531-012-0772-5, 2012.
Siebel, W., Hann, H. P., Danišík, M., Shang, C. K., Berthold, C., Rohrmüller, J., Wemmer, K., and Evans, N. J.: Age constraints on faulting and fault reactivation: a multi-chronological approach, Int. J. Earth Sci. (Geol. Rundsch.), 99, 1187–1197, https://doi.org/10.1007/s00531-009-0474-9, 2010.
Siebel, W., Shang, C. K., Reitter, E., Rohrmüller, J., and Breiter, K.: Two Distinctive Granite Suites in the Southwestern Bohemian Massif: Reply to F. Finger and M. René, J. Petrol, 50, 595–599, https://doi.org/10.1093/petrology/egp012, 2009.
Siebel, W., Shang, C. K., Reitter, E., Rohrmüller, J., and Breiter, K.: Two Distinctive Granite Suites in the SW Bohemian Massif and their Record of Emplacement: Constraints from Geochemistry and Zircon 207Pb/206Pb Chronology, J. Petrol, 49, 1853–1872, https://doi.org/10.1093/petrology/egn049, 2008.
Siebel, W., Thiel, M., and Chen, F.: Zircon geochronology and compositional record of late- to post-kinematic granitoids associated with the Bavarian Pfahl zone (Bavarian Forest), Mineral. Petrol., 86, 45–62, https://doi.org/10.1007/s00710-005-0091-7, 2006a.
Siebel, W., Hann, H. P., Shang, C. K., Rohrmüller, J., and Chen, F.: Coeval late-Variscan emplacement of granitic rocks: an example from the Regensburg Forest, NE Bavaria, N. Jb. Miner. Abh., 183, 13–26, https://doi.org/10.1127/0077-7757/2006/0058, 2006b.
Siebel, W., Blaha, U., Chen, F., and Rohrmüller, J.: Geochronology and geochemistry of a dyke-host rock association and implications for the formation of the Bavarian Pfahl shear zone, Bohemian Massif, Int. J. Earth Sci. (Geol. Rundsch.), 94, 8–23, https://doi.org/10.1007/s00531-004-0445-0, 2005.
Siebel, W., Chen, F., and Satir, M.: Late-Variscan magmatism revisited: new implications from Pb-evaporation zircon ages on the emplacement of redwitzites and granites in NE Bavaria, Int. J. Earth Sci. (Geol. Rundsch.), 92, 36–53, https://doi.org/10.1007/s00531-002-0305-8, 2003.
Siebel, W., Trzebski, R., Stettner, G., Hecht, L., Casten, U., Höhndorf, A., and Müller, P.: Granitoid magmatism of the NW Bohemian Massif revealed: gravity data, composition, age relations and phase concept, Int. J. Earth Sci. (Geol. Rundsch.), 86, 45–63, https://doi.org/10.1007/PL00014665, 1997.
Skiba, P.: Homogene Schwerekarte der Bundesrepublik Deutschland (Bouguer-Anomalien). Technischer Bericht zur Fortführung der Datenbasis, deren Auswertung und Visualisierung, LIAG-Bericht, Hannover, 88 pp., 2011.
Smithson, S. B.: Densities of metamorphic rocks, Geophysics, 36, 690–694, https://doi.org/10.1190/1.1440205, 1971.
Stephan, T., Kroner, U., Hahn, T., Hallas, P., and Heuse, T.: Fold/cleavage relationships as indicator for late Variscan sinistral transpression at the Rheno-Hercynian–Saxo-Thuringian boundary zone, Central European Variscides, Tectonophysics, 681, 250–262, https://doi.org/10.1016/j.tecto.2016.03.005, 2016.
Stettner, G.: Zur geologisch-tektonischen Entwicklung des Oberpfälzer Grundgebirges, Der Aufschluß, 26, 11–38, 1975.
Stewart, I. S. and Hancock, P. L.: What is a fault scarp?, Episodes, 13, 256–263, 1990.
Teipel, U., Galadí-Enríquez, E., Glaser, S., Kroemer, E., and Rohrmüller, J.: Geologische Karte des Bayerischen Waldes 1:150000, Bayerisches Landesamt für Umwelt, Augsburg, 21 pp., 2008.
Telbisz, T., Kovács, G., Székely, B., and Szabó, J.: Topographic swath profile analysis: a generalization and sensitivity evaluation of a digital terrain analysis tool, Z. Geomorphol., 57, 485–513, https://doi.org/10.1127/0372-8854/2013/0110, 2013.
Toloczyki, M., Trurnit, P., Voges, A., Wittekindt, H., and Zitzmann, A.: Geologische Karte der Bundesrepublik Deutschland 1:1.000.000 (GK1000), Bundesanstalt für Geowissenschaften und Rohstoffe, Hannover, 2006.
Troll, G.: Die blastokataklastischen Kristallingesteine der Stallwanger Furche, Bayerischer Wald, in: Geologica Bavarica Nr. 58: Führer zu geologisch-petrographischen Exkursionen im Bayerischen Wald, edited by: Bayerisches Geologisches Landesamt, München, 22–33, 1967.
Trzebski, R., Behr, H. J., and Conrad, W.: Subsurface distribution and tectonic setting of the late-Variscan granites in the northwestern Bohemian Massif, Int. J. Earth Sci. (Geol. Rundsch.), 86, 64–78, https://doi.org/10.1007/PL00014666, 1997.
Unger, H. J. and Risch, H.: Die Thermalwasserbohrung Straubing Th 1 und ihr geologischer Rahmen, Geol. Jb., A, 3–51, 1991.
Vamvaka, A., Siebel, W., Chen, F., and Rohrmüller, J.: Apatite fission-track dating and low-temperature history of the Bavarian Forest (southern Bohemian Massif), Int. J. Earth Sci. (Geol. Rundsch.), 103, 103–119, https://doi.org/10.1007/s00531-013-0945-x, 2014.
Vercoutere, C.: The Thermotectonic History of the Brabant Massif (Belgium) and the Naab Basement (Germany): an Apatite Fission Track Analysis, PhD thesis, Faculteit Wetenschappen, Universiteit Gent, Gent, 191 pp., 1994.
Voigt, T., Kley, J., and Voigt, S.: Dawn and dusk of Late Cretaceous basin inversion in central Europe, Solid Earth, 12, 1443–1471, https://doi.org/10.5194/se-12-1443-2021, 2021.
von Eynatten, H., Kley, J., Dunkl, I., Hoffmann, V.-E., and Simon, A.: Late Cretaceous to Paleogene exhumation in central Europe – localized inversion vs. large-scale domal uplift, Solid Earth, 12, 935–958, https://doi.org/10.5194/se-12-935-2021, 2021.
Wagner, G. A., Coyle, D. A., Duyster, J., Henjes-Kunst, F., Peterek, A., Schröder, B., Stöckhert, B., Wemmer, K., Zulauf, G., Ahrendt, H., Bischoff, R., Hejl, E., Jacobs, J., Menzel, D., Nand Lal, Van den Haute, P., Vercoutere, C., and Welzel, B.: Post-Variscan thermal and tectonic evolution of the KTB site and its surroundings, J. Geophys. Res., 102, 18221–18232, https://doi.org/10.1029/96JB02565, 1997.
Wagner, G. A., Michalski, I., and Zaun, P.: Apatite Fission Track Dating of the Central European Basement. Postvariscan Thermo-Tectonic Evolution, in: The German continental deep drilling program (KTB): Site selection studies in the Oberpfalz and Schwarzwald, edited by: Emmermann, R. and Wohlenberg, J., Springer, Berlin, Heidelberg, New York, London, Paris, Tokyo, Hong Kong, 481–500, 1989.
Wallbrecher, E., Dallmeyer, R. D., Brandmayr, M., Handler, R., Maderbacher, F., and Platzer, R.: Kinematik und Alter der Blattverschiebungszonen in der südlichen Böhmischen Masse, in: Arbeitstagung Geol. B.-A., edited by: Gattiner, T. E. and Roetzel, R., Verlag d. Geologischen Bundesanstalt, 35–48, 1991.
Weinberg, R. F., Sial, A. N., and Mariano, G.: Close spatial relationship between plutons and shear zones, Geology, 32, 377–380, https://doi.org/10.1130/G20290.1, 2004.
Welzel, B.: Die Bedeutung von K-/Ar-Datierungen an detritischen Muskoviten fur die Rekonstruktion tektonometamorpher Einheiten im orogenen Liefergebiet – ein Beitrag zur Frage der variskischen Krustenentwicklung in der Böhmischen Masse, Göttinger Arb. Geol. Paläont., 61 pp., 1991.
Wimmenauer, W. and Bryhni, I.: A systematic nomenclature for metamorphic rocks: Migmatites and related rocks, A proposal on behalf of the IUGS Subcommission on the Systematics of Metamorphic Rocks, Web version of 01.02.2007, 5 pp., 2007.
Winter, J. D.: An introduction to igneous and metamorphic petrology, 2. ed., Prentice Hall, Upper Saddle River, NJ, 702 pp., 2010.
Žák, J. and Sláma, J.: How far did the Cadomian 'terranes' travel from Gondwana during early Palaeozoic? A critical reappraisal based on detrital zircon geochronology, Int. Geol. Rev., 60, 319–338, https://doi.org/10.1080/00206814.2017.1334599, 2018.
Žák, J., Verner, K., Janoušek, V., Holub, F. V., Kachlík, V., Finger, F., Hajná, J., Tomek, F., Vondrovic, L., and Trubač, J.: A plate-kinematic model for the assembly of the Bohemian Massif constrained by structural relationships around granitoid plutons, Geol. Soc. Spec. Publ., 405, 169–196, https://doi.org/10.1144/SP405.9, 2014.
Zeitlhöfler, M., Wagner, B., and Spörlein, T.: Geologica Bavarica Nr. 112: Strukturgeologie und Grundwasserführung im ostbayerischen Grundgebirge, Augsburg, 64 pp., 2015.
Zeitlhöfler, M.: Brittle Petrofabrics in the Central Bavarian Forest (SE Germany): Tectonic Evolution, Geomorphological Effects, and Hydrogeologic Implications, PhD thesis, Fakultät für Geowissenschaften, Ludwig-Maximilians-Universität München, München, 249 pp., 2007.
Ziegler, P. A.: Late Cretaceous and Cenozoic intra-plate compressional deformations in the Alpine foreland – a geodynamic model, Tectonophysics, 137, 389–420, https://doi.org/10.1016/0040-1951(87)90330-1, 1987.
Ziegler, P. A., Cloetingh, S., and van Wees, J.-D.: Dynamics of intra-plate compressional deformation: the Alpine foreland and other examples, Tectonophysics, 252, 7–59, https://doi.org/10.1016/0040-1951(95)00102-6, 1995.
- Full-text XML
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.
We combine gravity anomaly and topographic data with observations from thermochronology,...