Articles | Volume 16, issue 7
https://doi.org/10.5194/se-16-619-2025
© Author(s) 2025. 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-16-619-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
10 Jul 2025
Research article | Highlight paper |
| 10 Jul 2025
| 10 Jul 2025
Evidence for multi-rifting in the Variscan–Alpine cycle transition: insights from the European western Southern Alps
Emanuele Scaramuzzo
Department of Science and High Technology, University of Insubria, via Valleggio 11, 22100 Como, Italy
Franz A. Livio
Department of Science and High Technology, University of Insubria, via Valleggio 11, 22100 Como, Italy
Maria Giuditta Fellin
CORRESPONDING AUTHOR
Department of Earth and Planetary Sciences, ETH Zürich, Sonneggstrasse 5, 8092 Zurich, Switzerland
Colin Maden
Department of Earth and Planetary Sciences, ETH Zürich, Sonneggstrasse 5, 8092 Zurich, Switzerland
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Franz A. Livio, Anna M. Blumetti, Valerio Comerci, Francesca Ferrario, Gilberto Binda, Marco Caciagli, Michela Colombo, Pio Di Manna, Fernando Ferri, Fiorenzo Fumanti, Roberto Gambillara, Maurizio Guerra, Luca Guerrieri, Paolo Lorenzoni, Valerio Materni, Francesco Miscione, Rosa Nappi, Rosella Nave, Kathleen Nicoll, Alba Peiro, Marco Pizza, Roberto Pompili, Luca M. Puzzilli, Mauro Roma, Aurora Rossi, Valerio Ruscito, Vincenzo Sapia, Argelia Silva Fragoso, Emanuele Scaramuzzo, Frank Thomas, Giorgio Tringali, Stefano Urbini, Andrea Zerboni, and Alessandro M. Michetti
EGUsphere, https://doi.org/10.5194/egusphere-2025-2531, https://doi.org/10.5194/egusphere-2025-2531, 2025
This preprint is open for discussion and under review for Natural Hazards and Earth System Sciences (NHESS).
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The Rieti Basin in Central Italy, though surrounded by active faults, has been largely overlooked in earthquake studies. To better understand its seismic past, we dug 17 trenches and discovered evidence of 15 ancient earthquakes over the past ca. 20,000 years. The findings show that earthquakes in this area tend to cluster in time, likely due to stress shifting between nearby faults, and can reach a magnitude of 6.5.
Franz A. Livio, Anna M. Blumetti, Valerio Comerci, Francesca Ferrario, Gilberto Binda, Marco Caciagli, Michela Colombo, Pio Di Manna, Fernando Ferri, Fiorenzo Fumanti, Roberto Gambillara, Maurizio Guerra, Luca Guerrieri, Paolo Lorenzoni, Valerio Materni, Francesco Miscione, Rosa Nappi, Rosella Nave, Kathleen Nicoll, Alba Peiro, Marco Pizza, Roberto Pompili, Luca M. Puzzilli, Mauro Roma, Aurora Rossi, Valerio Ruscito, Vincenzo Sapia, Argelia Silva Fragoso, Emanuele Scaramuzzo, Frank Thomas, Giorgio Tringali, Stefano Urbini, Andrea Zerboni, and Alessandro M. Michetti
EGUsphere, https://doi.org/10.5194/egusphere-2025-2531, https://doi.org/10.5194/egusphere-2025-2531, 2025
This preprint is open for discussion and under review for Natural Hazards and Earth System Sciences (NHESS).
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The Rieti Basin in Central Italy, though surrounded by active faults, has been largely overlooked in earthquake studies. To better understand its seismic past, we dug 17 trenches and discovered evidence of 15 ancient earthquakes over the past ca. 20,000 years. The findings show that earthquakes in this area tend to cluster in time, likely due to stress shifting between nearby faults, and can reach a magnitude of 6.5.
Alberto Mariani, Jacopo Borsotti, Franz Livio, Giacomo Villa, Martin Metzger, and Fabiano Monti
EGUsphere, https://doi.org/10.31223/X5972C, https://doi.org/10.31223/X5972C, 2025
This preprint is open for discussion and under review for The Cryosphere (TC).
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We developed a new model to estimate snow depth using radar satellite data. By correcting for how the viewing angle affects signal reflection, we reduced errors by nearly 40 %. Tested in the Alps and Norway, the method improves fine-scale snow monitoring, supporting avalanche forecasting and water management.
Giorgio Tringali, Domenico Bella, Franz Livio, Anna Maria Blumetti, Gianluca Groppelli, Luca Guerrieri, Marco Neri, Vincenzo Adorno, Rosario Pettinato, Sara Trotta, and Alessandro M. Michetti
EGUsphere, https://doi.org/10.5194/egusphere-2024-4078, https://doi.org/10.5194/egusphere-2024-4078, 2025
This preprint is open for discussion and under review for Solid Earth (SE).
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Trenches were excavated to provide data for relocating buildings damaged by the 2018 earthquake on Mt. Etna. The paleoseismological results along the Fiandaca Fault revealed 3 surface faulting events occurred in: 2018, 1894 and another unknown one in the Early Middle Ages. To verify an increasing trend in seismicity, fault scarps were analysed obtaining movements over different timescales, starting from 115000 years ago, suggesting a very recent growth in flank instability on Etna eastern flank.
Franz Livio, Maria Francesca Ferrario, Elisa Martinelli, Sahra Talamo, Silvia Cercatillo, and Alessandro Maria Michetti
Nat. Hazards Earth Syst. Sci., 23, 3407–3424, https://doi.org/10.5194/nhess-23-3407-2023, https://doi.org/10.5194/nhess-23-3407-2023, 2023
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Here we document the occurrence of an historical earthquake that occurred in the European western Southern Alps in the sixth century CE. Analysis of the effects due to earthquake shaking in the city of Como (N Italy) and a comparison with dated offshore landslides in the Alpine lakes allowed us to make an inference about the possible magnitude and the location of the seismic source for this event.
Erica D. Erlanger, Maria Giuditta Fellin, and Sean D. Willett
Solid Earth, 13, 347–365, https://doi.org/10.5194/se-13-347-2022, https://doi.org/10.5194/se-13-347-2022, 2022
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We present an erosion rate analysis on dated rock and sediment from the Northern Apennine Mountains, Italy, which provides new insights on the pattern of erosion rates through space and time. This analysis shows decreasing erosion through time on the Ligurian side but increasing erosion through time on the Adriatic side. We suggest that the pattern of erosion rates is consistent with the present asymmetric topography in the Northern Apennines, which has likely existed for several million years.
Maria Francesca Ferrario and Franz Livio
Solid Earth, 12, 1197–1209, https://doi.org/10.5194/se-12-1197-2021, https://doi.org/10.5194/se-12-1197-2021, 2021
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Moderate to strong earthquakes commonly produce surface faulting, either along the primary fault or as distributed rupture on nearby faults. Hazard assessment for distributed normal faulting is based on empirical relations derived almost 15 years ago. In this study, we derive updated empirical regressions of the probability of distributed faulting as a function of distance from the primary fault, and we propose a conservative scenario to consider the full spectrum of potential rupture.
Lydia R. Bailey, Filippo L. Schenker, Maria Giuditta Fellin, Miriam Cobianchi, Thierry Adatte, and Vincenzo Picotti
Solid Earth, 11, 2463–2485, https://doi.org/10.5194/se-11-2463-2020, https://doi.org/10.5194/se-11-2463-2020, 2020
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The Kallipetra Basin, formed in the Late Cretaceous on the reworked Pelagonian–Axios–Vardar contact in the Hellenides, is described for the first time. We document how and when the basin evolved in response to tectonic forcings and basin inversion. Cenomanian extension and basin widening was followed by Turonian compression and basin inversion. Thrusting occurred earlier than previously reported in the literature, with a vergence to the NE, at odds with the regional SW vergence of the margin.
F. L. Schenker, M. G. Fellin, and J.-P. Burg
Solid Earth, 6, 285–302, https://doi.org/10.5194/se-6-285-2015, https://doi.org/10.5194/se-6-285-2015, 2015
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The eastern Mediterranean is a long-lived seismically active region where the interaction of compressive and extensive tectonics is responsible for complex crustal deformation. The Pelagonian zone in the Hellenides has witnessed such deformational processes since the Mesozoic. This study combines fission-track analysis (recording temperatures <240°C), structural and stratigraphic data that were essential to constrain the polyphase evolution of the Hellenic orogen over 100 Ma.
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
Importance of forearc topography for the triggering of aftershocks of megathrust earthquakes: insights from mechanical models and the Tohoku-Oki and Maule earthquakes
About the trustworthiness of physics-based machine learning – considerations for geomechanical applications
Relict landscape evolution and fault reactivation in the eastern Tian Shan: insights from the Harlik Mountains
Switching extensional and contractional tectonics in the West Kunlun Mountains during the Jurassic period: responses to the Neo-Tethyan geodynamics along the Eurasian margin
Seismo-tectonics of Greater Iberia: An updated review
Influence of lateral heterogeneities on strike-slip fault behaviour: insights from analogue models
Importance of basement faulting and salt decoupling for the structural evolution of the Fars Arc (Zagros fold-and-thrust belt): a numerical modeling approach
Low-temperature thermochronology and its geological significance in the central and northern section of the western margin of the Ordos Basin
On the role of trans-lithospheric faults in the long-term seismotectonic segmentation of active margins: a case study in the Andes
Along-strike variation in volcanic addition controlling post-breakup sedimentary infill: Pelotas margin, austral South Atlantic
Stress state at faults: the influence of rock stiffness contrast, stress orientation, and ratio
Interseismic and long-term deformation of southeastern Sicily driven by the Ionian slab roll-back
Rift and plume: a discussion on active and passive rifting mechanisms in the Afro-Arabian rift based on synthesis of geophysical data
Propagating rifts: the roles of crustal damage and ascending mantle fluids
Cretaceous–Paleocene extension at the southwestern continental margin of India and opening of the Laccadive basin: constraints from geophysical data
Extensional exhumation of cratons: insights from the Early Cretaceous Rio Negro–Juruena belt (Amazonian Craton, Colombia)
Hydrogen solubility of stishovite provides insights into water transportation to the deep Earth
Networks of geometrically coherent faults accommodate Alpine tectonic inversion offshore southwestern Iberia
Melt-enhanced strain localization and phase mixing in a large-scale mantle shear zone (Ronda peridotite, Spain)
Selective inversion of rift basins in lithospheric-scale analogue experiments
The link between Somalian Plate rotation and the East African Rift System: an analogue modelling study
Inversion of extensional basins parallel and oblique to their boundaries: inferences from analogue models and field observations from the Dolomites Indenter, European eastern Southern Alps
Magnetic fabric analyses of basin inversion: a sandbox modelling approach
The influence of crustal strength on rift geometry and development – insights from 3D numerical modelling
Construction of the Ukrainian Carpathian wedge from low-temperature thermochronology and tectono-stratigraphic analysis
Analogue modelling of basin inversion: a review and future perspectives
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Tectonostratigraphic evolution of the Slyne Basin
Control of crustal strength, tectonic inheritance, and stretching/ shortening rates on crustal deformation and basin reactivation: insights from laboratory models
Late Cretaceous–early Palaeogene inversion-related tectonic structures at the northeastern margin of the Bohemian Massif (southwestern Poland and northern Czechia)
The analysis of slip tendency of major tectonic faults in Germany
Earthquake ruptures and topography of the Chilean margin controlled by plate interface deformation
Late Quaternary faulting in the southern Matese (Italy): implications for earthquake potential and slip rate variability in the southern Apennines
Rare earth elements associated with carbonatite–alkaline complexes in western Rajasthan, India: exploration targeting at regional scale
Structural complexities and tectonic barriers controlling recent seismic activity in the Pollino area (Calabria–Lucania, southern Italy) – constraints from stress inversion and 3D fault model building
The Mid Atlantic Appalachian Orogen Traverse: a comparison of virtual and on-location field-based capstone experiences
Chronology of thrust propagation from an updated tectono-sedimentary framework of the Miocene molasse (western Alps)
Orogenic lithosphere and slabs in the greater Alpine area – interpretations based on teleseismic P-wave tomography
Ground-penetrating radar signature of Quaternary faulting: a study from the Mt. Pollino region, southern Apennines, Italy
U–Pb dating of middle Eocene–Pliocene multiple tectonic pulses in the Alpine foreland
Detrital zircon provenance record of the Zagros mountain building from the Neotethys obduction to the Arabia–Eurasia collision, NW Zagros fold–thrust belt, Kurdistan region of Iraq
The Subhercynian Basin: an example of an intraplate foreland basin due to a broken plate
Late to post-Variscan basement segmentation and differential exhumation along the SW Bohemian Massif, central Europe
Holocene surface-rupturing earthquakes on the Dinaric Fault System, western Slovenia
Contribution of gravity gliding in salt-bearing rift basins – a new experimental setup for simulating salt tectonics under the influence of sub-salt extension and tilting
Thick- and thin-skinned basin inversion in the Danish Central Graben, North Sea – the role of deep evaporites and basement kinematics
Complex rift patterns, a result of interacting crustal and mantle weaknesses, or multiphase rifting? Insights from analogue models
Interactions of plutons and detachments: a comparison of Aegean and Tyrrhenian granitoids
Insights from elastic thermobarometry into exhumation of high-pressure metamorphic rocks from Syros, Greece
Stress rotation – impact and interaction of rock stiffness and faults
Armin Dielforder, Gian Maria Bocchini, and Andrea Hampel
Solid Earth, 16, 593–618, https://doi.org/10.5194/se-16-593-2025, https://doi.org/10.5194/se-16-593-2025, 2025
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Subduction zones feature a large elevation difference between the deep oceanic trench and the high mountains on land, which causes stress in the upper plate. We investigate how the topographic stress affects the aftershock seismicity of large subduction earthquakes using analytical and numerical stress models. We show that topographic stress has a large influence on aftershock seismicity and promoted most of the seismicity after the Tohoku-Oki (Japan) and Maule (Chile) earthquakes.
Denise Degen, Moritz Ziegler, Oliver Heidbach, Andreas Henk, Karsten Reiter, and Florian Wellmann
Solid Earth, 16, 477–502, https://doi.org/10.5194/se-16-477-2025, https://doi.org/10.5194/se-16-477-2025, 2025
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Obtaining reliable estimates of the subsurface state distributions is essential to determine the location of, e.g., potential nuclear waste disposal sites. However, providing these is challenging since it requires solving the problem numerous times, yielding high computational cost. To overcome this, we use a physics-based machine learning method to construct surrogate models. We demonstrate how it produces physics-preserving predictions, which differentiates it from purely data-driven approaches.
Zihao Zhao, Tianyi Shen, Guocan Wang, Peter van der Beek, Yabo Zhou, and Cheng Ma
Solid Earth, 16, 503–530, https://doi.org/10.5194/se-16-503-2025, https://doi.org/10.5194/se-16-503-2025, 2025
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This study examines the evolution of the Harlik Mountains in the eastern Tian Shan. Low-relief surfaces were formed by the Early Cretaceous erosion and subsequent tectonic stability. Later fault activity segmented these surfaces, with uplift and tilting in the Cenozoic driven by tectonic reactivation. These findings provide insights into how landscapes evolve in response to geological and environmental changes over millions of years.
Hong-Xiang Wu, Han-Lin Chen, Andrew V. Zuza, Yildirim Dilek, Du-Wei Qiu, Qi-Ye Lu, Feng-Qi Zhang, Xiao-Gan Cheng, and Xiu-Bin Lin
Solid Earth, 16, 155–177, https://doi.org/10.5194/se-16-155-2025, https://doi.org/10.5194/se-16-155-2025, 2025
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The Tethyan orogenic belt records an extensive history of subduction along the southern margin of Eurasia. We examine the magmatism, stratigraphy, and sedimentary provenance of the Jurassic basin in the West Kunlun Mountains, highlighting the switching extensional and contractional tectonic episodes in central Asia. The complex evolution was related to the subduction of the Neo-Tethys Ocean, transitioning from southward retreat to northward flat-slab advancement.
Antonio J. Olaiz, José A. Álvarez Gómez, Gerardo de Vicente, Alfonso Muñoz-Martín, Juan V. Cantavella, Susana Custódio, Dina Vales, and Oliver Heidbach
EGUsphere, https://doi.org/10.5194/egusphere-2024-4126, https://doi.org/10.5194/egusphere-2024-4126, 2025
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Understanding the stress and strain conditions in the Earth crust is crucial for various activities, such as oil and gas exploration and assessing seismic hazards. In this article, we have updated the database of moment tensor focal mechanisms for the Greater Iberia. We conducted kinematic and dynamic analyses on the selected populations, determining the average focal mechanism, strain and stress orientations, and tectonic regime. The orientation for horizontal compression is primarily N154° E.
Sandra González-Muñoz, Guido Schreurs, Timothy C. Schmid, and Fidel Martín-González
Solid Earth, 15, 1509–1523, https://doi.org/10.5194/se-15-1509-2024, https://doi.org/10.5194/se-15-1509-2024, 2024
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This work investigates how strike-slip faults propagate across domains with lateral contrasting brittle strength using analogue models. The introduction of brittle vertical domains was achieved using quartz microbead sand. The reference vertical domains influence synthetic fault propagation, segmentation, and linkage, as well as the antithetic faults which rotate about a vertical axis due to the applied simple shear. The results aligned with the faults in the NW of the Iberian Peninsula.
Fatemeh Gomar, Jonas B. Ruh, Mahdi Najafi, and Farhad Sobouti
Solid Earth, 15, 1479–1507, https://doi.org/10.5194/se-15-1479-2024, https://doi.org/10.5194/se-15-1479-2024, 2024
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Our study investigates the structural evolution of the Fars Arc in the Zagros Mountains through numerical modeling. We focus on the effects of the interaction between basement faults and salt décollement levels during tectonic inversion, including a rifting and a convergence phase. In conclusion, our results emphasize the importance of considering fault geometry, salt rheology, and basement involvement in understanding the resistance to deformation and the seismic behavior of fold–thrust belts.
Guangyuan Xing, Zhanli Ren, Kai Qi, Sasa Guo, Yanzhao Liu, Ying Zhang, and Huaping Lan
EGUsphere, https://doi.org/10.5194/egusphere-2024-3191, https://doi.org/10.5194/egusphere-2024-3191, 2024
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In this study, we accurately constrain the uplift and cooling history of the central and northern western Ordos Basin using apatite fission tracks and (U-Th)/He dating methods, and reveal significant differences in the timing and intensity of uplift in different regions. These findings highlight spatial differences in the timing and rate of uplift in the western Ordos Basin. This suggests that the Yanshan orogenic movement had the most significant tectonic influence on the study area.
Gonzalo Yanez C., Jose Piquer R., and Orlando Rivera H.
Solid Earth, 15, 1319–1342, https://doi.org/10.5194/se-15-1319-2024, https://doi.org/10.5194/se-15-1319-2024, 2024
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We postulate that the observed spatial distribution of large earthquakes in active convergence zones, organised in segments where large events are repeated every 100–300 years, depends on large-scale continental faults and fluid release from the subducting slab. In order to support this model, we use proxies at different spatial and temporal scales (historic seismicity, megathrust slip solutions, inter-seismic cumulative seismicity, GPS/viscous plate coupling, and coastline morphology).
Marlise C. Cassel, Nick Kusznir, Gianreto Manatschal, and Daniel Sauter
Solid Earth, 15, 1265–1279, https://doi.org/10.5194/se-15-1265-2024, https://doi.org/10.5194/se-15-1265-2024, 2024
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We investigate the along-strike variation in volcanics on the Pelotas segment of the Brazilian margin created during continental breakup and formation of the southern South Atlantic. We show that the volume of volcanics strongly controls the amount of space available for post-breakup sedimentation. We also show that breakup varies along-strike from very magma-rich to magma-normal within a relatively short distance of less than 300 km. This is not as expected from a simple mantle plume model.
Moritz O. Ziegler, Robin Seithel, Thomas Niederhuber, Oliver Heidbach, Thomas Kohl, Birgit Müller, Mojtaba Rajabi, Karsten Reiter, and Luisa Röckel
Solid Earth, 15, 1047–1063, https://doi.org/10.5194/se-15-1047-2024, https://doi.org/10.5194/se-15-1047-2024, 2024
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The rotation of the principal stress axes in a fault structure because of a rock stiffness contrast has been investigated for the impact of the ratio of principal stresses, the angle between principal stress axes and fault strike, and the ratio of the rock stiffness contrast. A generic 2D geomechanical model is employed for the systematic investigation of the parameter space.
Amélie Viger, Stéphane Dominguez, Stéphane Mazzotti, Michel Peyret, Maxime Henriquet, Giovanni Barreca, Carmelo Monaco, and Adrien Damon
Solid Earth, 15, 965–988, https://doi.org/10.5194/se-15-965-2024, https://doi.org/10.5194/se-15-965-2024, 2024
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New satellite geodetic data (PS-InSAR) evidence a generalized subsidence and an eastward tilting of southeastern Sicily combined with a local relative uplift along its eastern coast. We perform flexural and elastic modeling and show that the slab pull force induced by the Ionian slab roll-back and extrado deformation reproduce the measured surface deformation. Finally, we propose an original seismic cycle model that is mainly driven by the southward migration of the Ionian slab roll-back.
Ran Issachar, Peter Haas, Nico Augustin, and Jörg Ebbing
Solid Earth, 15, 807–826, https://doi.org/10.5194/se-15-807-2024, https://doi.org/10.5194/se-15-807-2024, 2024
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In this contribution, we explore the causal relationship between the arrival of the Afar plume and the initiation of the Afro-Arabian rift. We mapped the rift architecture in the triple-junction region using geophysical data and reviewed the available geological data. We interpret a progressive development of the plume–rift system and suggest an interaction between active and passive mechanisms in which the plume provided a push force that changed the kinematics of the associated plates.
Folarin Kolawole and Rasheed Ajala
Solid Earth, 15, 747–762, https://doi.org/10.5194/se-15-747-2024, https://doi.org/10.5194/se-15-747-2024, 2024
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We investigate the upper-crustal structure of the Rukwa–Tanganyika rift zone in East Africa, where the Tanganyika rift interacts with the Rukwa and Mweru-Wantipa rifts, coinciding with abundant seismicity at the rift tips. Seismic velocity structure and patterns of seismicity clustering reveal zones around 10 km deep with anomalously high Vp / Vs ratios at the rift tips, indicative of a localized mechanically weakened crust caused by mantle volatiles and damage associated with bending strain.
Mathews George Gilbert, Parakkal Unnikrishnan, and Munukutla Radhakrishna
Solid Earth, 15, 671–682, https://doi.org/10.5194/se-15-671-2024, https://doi.org/10.5194/se-15-671-2024, 2024
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The study identifies evidence for extension south of Tellicherry Arch along the southwestern continental margin of India through the integrated analysis of multichannel seismic and gravity data. The sediment deposition pattern indicates that this extension occurred after the Eocene. We further propose that the anticlockwise rotation of India and the passage of the Réunion plume have facilitated the opening of the Laccadive basin.
Ana Fonseca, Simon Nachtergaele, Amed Bonilla, Stijn Dewaele, and Johan De Grave
Solid Earth, 15, 329–352, https://doi.org/10.5194/se-15-329-2024, https://doi.org/10.5194/se-15-329-2024, 2024
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This study explores the erosion and exhumation processes and history of early continental crust hidden within the Amazonian Rainforest. This crust forms part of the Amazonian Craton, an ancient continental fragment. Our surprising findings reveal the area underwent rapid early Cretaceous exhumation triggered by tectonic forces. This discovery challenges the traditional perception that cratons are stable and long-lived entities and shows they can deform readily under specific geological contexts.
Mengdan Chen, Changxin Yin, Danling Chen, Long Tian, Liang Liu, and Lei Kang
Solid Earth, 15, 215–227, https://doi.org/10.5194/se-15-215-2024, https://doi.org/10.5194/se-15-215-2024, 2024
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Stishovite remains stable under mantle conditions and can incorporate various amounts of water in its crystal structure. We provide a systematic review of previous studies on water in stishovite and propose a new model for water solubility of Al-bearing stishovite. Calculation results based on this model suggest that stishovite may effectively accommodate water from the breakdown of hydrous minerals and could make an important contribution to water enrichment in the mantle transition zone.
Tiago M. Alves
Solid Earth, 15, 39–62, https://doi.org/10.5194/se-15-39-2024, https://doi.org/10.5194/se-15-39-2024, 2024
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Alpine tectonic inversion is reviewed for southwestern Iberia, known for its historical earthquakes and tsunamis. High-quality 2D seismic data image 26 faults mapped to a depth exceeding 10 km. Normal faults accommodated important vertical uplift and shortening. They are 100–250 km long and may generate earthquakes with Mw > 8.0. Regions of Late Mesozoic magmatism comprise thickened, harder crust, forming lateral buttresses to compression and promoting the development of fold-and-thrust belts.
Sören Tholen, Jolien Linckens, and Gernold Zulauf
Solid Earth, 14, 1123–1154, https://doi.org/10.5194/se-14-1123-2023, https://doi.org/10.5194/se-14-1123-2023, 2023
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Intense phase mixing with homogeneously distributed secondary phases and irregular grain boundaries and shapes indicates that metasomatism formed the microstructures predominant in the shear zone of the NW Ronda peridotite. Amphibole presence, olivine crystal orientations, and the consistency to the Beni Bousera peridotite (Morocco) point to OH-bearing metasomatism by small fractions of evolved melts. Results confirm a strong link between reactions and localized deformation in the upper mantle.
Anindita Samsu, Weronika Gorczyk, Timothy Chris Schmid, Peter Graham Betts, Alexander Ramsay Cruden, Eleanor Morton, and Fatemeh Amirpoorsaeed
Solid Earth, 14, 909–936, https://doi.org/10.5194/se-14-909-2023, https://doi.org/10.5194/se-14-909-2023, 2023
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When a continent is pulled apart, it breaks and forms a series of depressions called rift basins. These basins lie above weakened crust that is then subject to intense deformation during subsequent tectonic compression. Our analogue experiments show that when a system of basins is squeezed in a direction perpendicular to the main trend of the basins, some basins rise up to form mountains while others do not.
Frank Zwaan and Guido Schreurs
Solid Earth, 14, 823–845, https://doi.org/10.5194/se-14-823-2023, https://doi.org/10.5194/se-14-823-2023, 2023
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The East African Rift System (EARS) is a major plate tectonic feature splitting the African continent apart. Understanding the tectonic processes involved is of great importance for societal and economic reasons (natural hazards, resources). Laboratory experiments allow us to simulate these large-scale processes, highlighting the links between rotational plate motion and the overall development of the EARS. These insights are relevant when studying other rift systems around the globe as well.
Anna-Katharina Sieberer, Ernst Willingshofer, Thomas Klotz, Hugo Ortner, and Hannah Pomella
Solid Earth, 14, 647–681, https://doi.org/10.5194/se-14-647-2023, https://doi.org/10.5194/se-14-647-2023, 2023
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Through analogue models and field observations, we investigate how inherited platform–basin geometries control strain localisation, style, and orientation of reactivated and new structures during inversion. Our study shows that the style of evolving thrusts and their changes along-strike are controlled by pre-existing rheological discontinuities. The results of this study are relevant for understanding inversion structures in general and for the European eastern Southern Alps in particular.
Thorben Schöfisch, Hemin Koyi, and Bjarne Almqvist
Solid Earth, 14, 447–461, https://doi.org/10.5194/se-14-447-2023, https://doi.org/10.5194/se-14-447-2023, 2023
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A magnetic fabric analysis provides information about the reorientation of magnetic grains and is applied to three sandbox models that simulate different stages of basin inversion. The analysed magnetic fabrics reflect the different developed structures and provide insights into the different deformed stages of basin inversion. It is a first attempt of applying magnetic fabric analyses to basin inversion sandbox models but shows the possibility of applying it to such models.
Thomas B. Phillips, John B. Naliboff, Ken J. W. McCaffrey, Sophie Pan, Jeroen van Hunen, and Malte Froemchen
Solid Earth, 14, 369–388, https://doi.org/10.5194/se-14-369-2023, https://doi.org/10.5194/se-14-369-2023, 2023
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Continental crust comprises bodies of varying strength, formed through numerous tectonic events. When subject to extension, these areas produce distinct rift and fault systems. We use 3D models to examine how rifts form above
strongand
weakareas of crust. We find that faults become more developed in weak areas. Faults are initially stopped at the boundaries with stronger areas before eventually breaking through. We relate our model observations to rift systems globally.
Marion Roger, Arjan de Leeuw, Peter van der Beek, Laurent Husson, Edward R. Sobel, Johannes Glodny, and Matthias Bernet
Solid Earth, 14, 153–179, https://doi.org/10.5194/se-14-153-2023, https://doi.org/10.5194/se-14-153-2023, 2023
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We study the construction of the Ukrainian Carpathians with LT thermochronology (AFT, AHe, and ZHe) and stratigraphic analysis. QTQt thermal models are combined with burial diagrams to retrieve the timing and magnitude of sedimentary burial, tectonic burial, and subsequent exhumation of the wedge's nappes from 34 to ∼12 Ma. Out-of-sequence thrusting and sediment recycling during wedge building are also identified. This elucidates the evolution of a typical wedge in a roll-back subduction zone.
Frank Zwaan, Guido Schreurs, Susanne J. H. Buiter, Oriol Ferrer, Riccardo Reitano, Michael Rudolf, and Ernst Willingshofer
Solid Earth, 13, 1859–1905, https://doi.org/10.5194/se-13-1859-2022, https://doi.org/10.5194/se-13-1859-2022, 2022
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When a sedimentary basin is subjected to compressional tectonic forces after its formation, it may be inverted. A thorough understanding of such
basin inversionis of great importance for scientific, societal, and economic reasons, and analogue tectonic models form a key part of our efforts to study these processes. We review the advances in the field of basin inversion modelling, showing how the modelling results can be applied, and we identify promising venues for future research.
Eleni Stavropoulou and Lyesse Laloui
Solid Earth, 13, 1823–1841, https://doi.org/10.5194/se-13-1823-2022, https://doi.org/10.5194/se-13-1823-2022, 2022
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Shales are identified as suitable caprock formations for geolocigal CO2 storage thanks to their low permeability. Here, small-sized shale samples are studied under field-representative conditions with X-ray tomography. The geochemical impact of CO2 on calcite-rich zones is for the first time visualised, the role of pre-existing micro-fissures in the CO2 invasion trapping in the matererial is highlighted, and the initiation of micro-cracks when in contact with anhydrous CO2 is demonstrated.
Conor M. O'Sullivan, Conrad J. Childs, Muhammad M. Saqab, John J. Walsh, and Patrick M. Shannon
Solid Earth, 13, 1649–1671, https://doi.org/10.5194/se-13-1649-2022, https://doi.org/10.5194/se-13-1649-2022, 2022
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The Slyne Basin is a sedimentary basin located offshore north-western Ireland. It formed through a long and complex evolution involving distinct periods of extension. The basin is subdivided into smaller basins, separated by deep structures related to the ancient Caledonian mountain-building event. These deep structures influence the shape of the basin as it evolves in a relatively unique way, where early faults follow these deep structures, but later faults do not.
Benjamin Guillaume, Guido M. Gianni, Jean-Jacques Kermarrec, and Khaled Bock
Solid Earth, 13, 1393–1414, https://doi.org/10.5194/se-13-1393-2022, https://doi.org/10.5194/se-13-1393-2022, 2022
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Under tectonic forces, the upper part of the crust can break along different types of faults, depending on the orientation of the applied stresses. Using scaled analogue models, we show that the relative magnitude of compressional and extensional forces as well as the presence of inherited structures resulting from previous stages of deformation control the location and type of faults. Our results gives insights into the tectonic evolution of areas showing complex patterns of deformation.
Andrzej Głuszyński and Paweł Aleksandrowski
Solid Earth, 13, 1219–1242, https://doi.org/10.5194/se-13-1219-2022, https://doi.org/10.5194/se-13-1219-2022, 2022
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Old seismic data recently reprocessed with modern software allowed us to study at depth the Late Cretaceous tectonic structures in the Permo-Mesozoic rock sequences in the Sudetes. The structures formed in response to Iberia collision with continental Europe. The NE–SW compression undulated the crystalline basement top and produced folds, faults and joints in the sedimentary cover. Our results are of importance for regional geology and in prospecting for deep thermal waters.
Luisa Röckel, Steffen Ahlers, Birgit Müller, Karsten Reiter, Oliver Heidbach, Andreas Henk, Tobias Hergert, and Frank Schilling
Solid Earth, 13, 1087–1105, https://doi.org/10.5194/se-13-1087-2022, https://doi.org/10.5194/se-13-1087-2022, 2022
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Reactivation of tectonic faults can lead to earthquakes and jeopardize underground operations. The reactivation potential is linked to fault properties and the tectonic stress field. We create 3D geometries for major faults in Germany and use stress data from a 3D geomechanical–numerical model to calculate their reactivation potential and compare it to seismic events. The reactivation potential in general is highest for NNE–SSW- and NW–SE-striking faults and strongly depends on the fault dip.
Nadaya Cubas, Philippe Agard, and Roxane Tissandier
Solid Earth, 13, 779–792, https://doi.org/10.5194/se-13-779-2022, https://doi.org/10.5194/se-13-779-2022, 2022
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Earthquake extent prediction is limited by our poor understanding of slip deficit patterns. From a mechanical analysis applied along the Chilean margin, we show that earthquakes are bounded by extensive plate interface deformation. This deformation promotes stress build-up, leading to earthquake nucleation; earthquakes then propagate along smoothed fault planes and are stopped by heterogeneously distributed deformation. Slip deficit patterns reflect the spatial distribution of this deformation.
Paolo Boncio, Eugenio Auciello, Vincenzo Amato, Pietro Aucelli, Paola Petrosino, Anna C. Tangari, and Brian R. Jicha
Solid Earth, 13, 553–582, https://doi.org/10.5194/se-13-553-2022, https://doi.org/10.5194/se-13-553-2022, 2022
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We studied the Gioia Sannitica normal fault (GF) within the southern Matese fault system (SMF) in southern Apennines (Italy). It is a fault with a long slip history that has experienced recent reactivation or acceleration. Present activity has resulted in late Quaternary fault scarps and Holocene surface faulting. The maximum slip rate is ~ 0.5 mm/yr. Activation of the 11.5 km GF or the entire 30 km SMF can produce up to M 6.2 or M 6.8 earthquakes, respectively.
Malcolm Aranha, Alok Porwal, Manikandan Sundaralingam, Ignacio González-Álvarez, Amber Markan, and Karunakar Rao
Solid Earth, 13, 497–518, https://doi.org/10.5194/se-13-497-2022, https://doi.org/10.5194/se-13-497-2022, 2022
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Rare earth elements (REEs) are considered critical mineral resources for future industrial growth due to their short supply and rising demand. This study applied an artificial-intelligence-based technique to target potential REE-deposit hosting areas in western Rajasthan, India. Uncertainties associated with the prospective targets were also estimated to aid decision-making. The presented workflow can be applied to similar regions elsewhere to locate potential zones of REE mineralisation.
Daniele Cirillo, Cristina Totaro, Giusy Lavecchia, Barbara Orecchio, Rita de Nardis, Debora Presti, Federica Ferrarini, Simone Bello, and Francesco Brozzetti
Solid Earth, 13, 205–228, https://doi.org/10.5194/se-13-205-2022, https://doi.org/10.5194/se-13-205-2022, 2022
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The Pollino region is a highly seismic area of Italy. Increasing the geological knowledge on areas like this contributes to reducing risk and saving lives. We reconstruct the 3D model of the faults which generated the 2010–2014 seismicity integrating geological and seismological data. Appropriate relationships based on the dimensions of the activated faults suggest that they did not fully discharge their seismic potential and could release further significant earthquakes in the near future.
Steven Whitmeyer, Lynn Fichter, Anita Marshall, and Hannah Liddle
Solid Earth, 12, 2803–2820, https://doi.org/10.5194/se-12-2803-2021, https://doi.org/10.5194/se-12-2803-2021, 2021
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Field trips in the Stratigraphy, Structure, Tectonics (SST) course transitioned to a virtual format in Fall 2020, due to the COVID pandemic. Virtual field experiences (VFEs) were developed in web Google Earth and were evaluated in comparison with on-location field trips via an online survey. Students recognized the value of VFEs for revisiting outcrops and noted improved accessibility for students with disabilities. Potential benefits of hybrid field experiences were also indicated.
Amir Kalifi, Philippe Hervé Leloup, Philippe Sorrel, Albert Galy, François Demory, Vincenzo Spina, Bastien Huet, Frédéric Quillévéré, Frédéric Ricciardi, Daniel Michoux, Kilian Lecacheur, Romain Grime, Bernard Pittet, and Jean-Loup Rubino
Solid Earth, 12, 2735–2771, https://doi.org/10.5194/se-12-2735-2021, https://doi.org/10.5194/se-12-2735-2021, 2021
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Molasse deposits, deposited and deformed at the western Alpine front during the Miocene (23 to 5.6 Ma), record the chronology of that deformation. We combine the first precise chronostratigraphy (precision of ∼0.5 Ma) of the Miocene molasse, the reappraisal of the regional structure, and the analysis of growth deformation structures in order to document three tectonic phases and the precise chronology of thrust westward propagation during the second one involving the Belledonne basal thrust.
Mark R. Handy, Stefan M. Schmid, Marcel Paffrath, Wolfgang Friederich, and the AlpArray Working Group
Solid Earth, 12, 2633–2669, https://doi.org/10.5194/se-12-2633-2021, https://doi.org/10.5194/se-12-2633-2021, 2021
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New images from the multi-national AlpArray experiment illuminate the Alps from below. They indicate thick European mantle descending beneath the Alps and forming blobs that are mostly detached from the Alps above. In contrast, the Adriatic mantle in the Alps is much thinner. This difference helps explain the rugged mountains and the abundance of subducted and exhumed units at the core of the Alps. The blobs are stretched remnants of old ocean and its margins that reach down to at least 410 km.
Maurizio Ercoli, Daniele Cirillo, Cristina Pauselli, Harry M. Jol, and Francesco Brozzetti
Solid Earth, 12, 2573–2596, https://doi.org/10.5194/se-12-2573-2021, https://doi.org/10.5194/se-12-2573-2021, 2021
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Past strong earthquakes can produce topographic deformations, often
memorizedin Quaternary sediments, which are typically studied by paleoseismologists through trenching. Using a ground-penetrating radar (GPR), we unveiled possible buried Quaternary faulting in the Mt. Pollino seismic gap region (southern Italy). We aim to contribute to seismic hazard assessment of an area potentially prone to destructive events as well as promote our workflow in similar contexts around the world.
Luca Smeraglia, Nathan Looser, Olivier Fabbri, Flavien Choulet, Marcel Guillong, and Stefano M. Bernasconi
Solid Earth, 12, 2539–2551, https://doi.org/10.5194/se-12-2539-2021, https://doi.org/10.5194/se-12-2539-2021, 2021
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In this paper, we dated fault movements at geological timescales which uplifted the sedimentary successions of the Jura Mountains from below the sea level up to Earth's surface. To do so, we applied the novel technique of U–Pb geochronology on calcite mineralizations that precipitated on fault surfaces during times of tectonic activity. Our results document a time frame of the tectonic evolution of the Jura Mountains and provide new insight into the broad geological history of the Western Alps.
Renas I. Koshnaw, Fritz Schlunegger, and Daniel F. Stockli
Solid Earth, 12, 2479–2501, https://doi.org/10.5194/se-12-2479-2021, https://doi.org/10.5194/se-12-2479-2021, 2021
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As continental plates collide, mountain belts grow. This study investigated the provenance of rocks from the northwestern segment of the Zagros mountain belt to unravel the convergence history of the Arabian and Eurasian plates. Provenance data synthesis and field relationships suggest that the Zagros Mountains developed as a result of the oceanic crust emplacement on the Arabian continental plate, followed by the Arabia–Eurasia collision and later uplift of the broader region.
David Hindle and Jonas Kley
Solid Earth, 12, 2425–2438, https://doi.org/10.5194/se-12-2425-2021, https://doi.org/10.5194/se-12-2425-2021, 2021
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Central western Europe underwent a strange episode of lithospheric deformation, resulting in a chain of small mountains that run almost west–east across the continent and that formed in the middle of a tectonic plate, not at its edges as is usually expected. Associated with these mountains, in particular the Harz in central Germany, are marine basins contemporaneous with the mountain growth. We explain how those basins came to be as a result of the mountains bending the adjacent plate.
Andreas Eberts, Hamed Fazlikhani, Wolfgang Bauer, Harald Stollhofen, Helga de Wall, and Gerald Gabriel
Solid Earth, 12, 2277–2301, https://doi.org/10.5194/se-12-2277-2021, https://doi.org/10.5194/se-12-2277-2021, 2021
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We combine gravity anomaly and topographic data with observations from thermochronology, metamorphic grades, and the granite inventory to detect patterns of basement block segmentation and differential exhumation along the southwestern Bohemian Massif. Based on our analyses, we introduce a previously unknown tectonic structure termed Cham Fault, which, together with the Pfahl and Danube shear zones, is responsible for the exposure of different crustal levels during late to post-Variscan times.
Christoph Grützner, Simone Aschenbrenner, Petra Jamšek
Rupnik, Klaus Reicherter, Nour Saifelislam, Blaž Vičič, Marko Vrabec, Julian Welte, and Kamil Ustaszewski
Solid Earth, 12, 2211–2234, https://doi.org/10.5194/se-12-2211-2021, https://doi.org/10.5194/se-12-2211-2021, 2021
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Several large strike-slip faults in western Slovenia are known to be active, but most of them have not produced strong earthquakes in historical times. In this study we use geomorphology, near-surface geophysics, and fault excavations to show that two of these faults had surface-rupturing earthquakes during the Holocene. Instrumental and historical seismicity data do not capture the strongest events in this area.
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.
Cited articles
Abramowitz, M. and Stegun, I. (Eds.): Handbook of Mathematical Functions, Dover Publications, New York, USA, ISBN 978-0-486-61272-0, 1970.
Allmendinger, R.: FaultKin 8 [code and data set], https://www.rickallmendinger.net/faultkin, last access: 3 April 2024.
Armienti, P., Corazzato, C., Groppelli, G., Natoli, E., and Pasquare, G.: Geological and petrographical study of Montecampione Triassic subvolcanic bodies (Southern Alps, Italy). Preliminary geodynamic results, B. Soc. Geol. Ital., 2, 67–78, 2003.
Baggio, P. and De Marco, L.: La serie basale tardo-paleozoica del Varesotto e le mineralizzazioni ad uranio della Valganna, Comitato nazionale per le ricerche nucleari – Studi Ricerche Divisione Geomineraria, 3, 15–103, 1960.
Bakos, F., Del Moro, A., and Visona, D.: The Hercynian volcano-phitonic association of Ganna (Lake Lugano, Central Southern Alps, Italy), Eur. J. Mineral., 2, 373–384, https://doi.org/10.1127/ejm/2/3/0373, 1990.
Barth, S., Oberli, F., and Meier, M.: Th-Pb versus U-Pb isotope systematics in allanite from co-genetic rhyolite and granodiorite: Implications for geochronology, Earth Planet. Sc. Lett., 124, 149–159, 1994.
Beltrando, M., Stockli, D. F., Decarlis, A., and Manatschal, G.: A crustal-scale view at rift localization along the fossil Adriatic margin of the Alpine Tethys preserved in NW Italy, Tectonics, 34, 1927–1951, https://doi.org/10.1002/2015TC003973, 2015.
Berger, A., Mercolli, I., Kapferer, N., and Fügenschuh, B.: Single and double exhumation of fault blocks in the internal Sesia-Lanzo Zone and the Ivrea-Verbano Zone (Biella, Italy), Int. J. Earth Sci., 101, 1877–1894, https://doi.org/10.1007/s00531-012-0755-6, 2012.
Bernoulli, D.: Zur Geologie des Monte Generoso: (Lombardische Alpen); ein Beitrag zur Kenntnis der südalpinen Sedimente, Beitr. Geol. Karte Schweiz, N. F., 118, 1–134, 1964.
Bernoulli, D.: The pre-Alpine geodynamic evolution of the Southern Alps: a short summary, Bulletin für angewandte Geologie, 12, 3–10, 2007.
Bernoulli, D., Ambrosi, C., Scapozza, C., Stockar, R., and Schenker, F., Gaggero, L., Antognini, M. and Bronzini, S.: Foglio 1373 Mendrisio (parte Est) con parte Ovest del foglio Como. – Atlante geologico della Svizzera 1: 25 000, Note esplicative, in: Ufficio federale di topografia, edited by: Dall'Agnolo, S., CH-3084 Wabern, ISBN 978-3-302-40077-8, 2018.
Berra, F., Galli, M. T., Reghellin, F., Torricelli, S., and Fantoni, R.: Stratigraphic evolution of the Triassic–Jurassic succession in the Western Southern Alps (Italy): the record of the two-stage rifting on the distal passive margin of Adria, Basin Res., 21, 335–353, https://doi.org/10.1111/j.1365-2117.2008.00384.x, 2009.
Berra, F., Tiepolo, M., Caironi, V., and Siletto, G. B.: U–Pb zircon geochronology of volcanic deposits from the Permian basin of the Orobic Alps (Southern Alps, Lombardy): chronostratigraphic and geological implications, Geol. Mag., 152, 429–443, https://doi.org/10.1017/S0016756814000405, 2015.
Berra, F., Felletti, F., and Tessarollo, A.: Stratigraphic Architecture of a Transtensional Continental Basin in Low-Latitude Semiarid Conditions: The Permian Succession of the Central Orobic Basin (Southern Alps, Italy), J. Sediment. Res., 86, 408–429, https://doi.org/10.2110/jsr.2016.26, 2016.
Bertotti, G., Picotti, V., Bernoulli, D., and Castellarin, A.: From rifting to drifting: tectonic evolution of the South-Alpine upper crust from the Triassic to the Early Cretaceous, Sediment. Geol., 86, 53–76, https://doi.org/10.1016/0037-0738(93)90133-P, 1993.
Bertotti, G., Seward, D., Wijbrans, J., Ter Voorde, M., and Hurford, A. J.: Crustal thermal regime prior to, during, and after rifting: A geochronological and modeling study of the Mesozoic South Alpine rifted margin, Tectonics, 18, 185–200, https://doi.org/10.1029/1998TC900028, 1999.
Bigi, G., Cosentino, D., Parotto, M., Sartori, R., and Scandone, P.: Structural Model of Italy Scale 1 V 500:000 – Consiglio 10 Nazionale delle Ricerche – Progetto Finalizzato Geodinamica, SELCA, Firenze, Italy, 1990.
Boehnke, P. and Harrison, T. M.: A meta-analysis of geochronologically relevant half-lives: what's the best decay constant?, Int. Geol. Rev., 56, 905–914, https://doi.org/10.1080/00206814.2014.908420, 2014.
Bonin, B., Brandlein, P., Bussy, F., Desmons, J., Eggenberger, U., Finger, F., Graf, K., Marro, C., Mercolli, I., Oberhänsli, R., Ploquin, A., Quadt von, A., Raumer von, J., Schaltegger, U., Steyrer, H.P., Visonà, D., and Vivier, G.: Late Varisican Magmatic Evolution of the Alpine Basement, in: The pre-Mesozoic Geology in the Alps, edited by: von Raumer, J., and Neubauer, F., Springer, Berlin, Germany, 169–199, https://doi.org/10.1007/978-3-642-84640-3, 1993.
Boriani, A. and Villa, I. M.: Geochronology of regional metamorphism in the Ivrea-Verbano zone and Serie dei Laghi, Italian Alps, Schweiz. Miner. Petrog., 77, 381–401, 1997.
Boriani, A., Burlini, L., and Sacchi, R.: The Cossato-Mergozzo-Brissago Line and the Pogallo Line (Southern Alps, Northern Italy) and their relationships with the late-Hercynian magmatic and metamorphic events, Tectonophysics, 182, 91–102, https://doi.org/10.1016/0040-1951(90)90344-8, 1990.
Boriani, A., Sassi, F., and Sassi, R.: The basement complexes in Italy, with special regards to those exposed in the Alps: a review, Episodes, 26, 186–192, https://doi.org/10.18814/epiiugs/2003/v26i3/006, 2003.
Brack, P. and Rieber, H.: Towards a better definition of the Anisian/Ladinian boundary: New biostratigraphic data and correlations of boundary sections from the Southern Alps, Eclogae Geol. Helv., 86, 415–527, 1993.
Cadel, G.: Geology and uranium mineralization of the Collio Basin (central Southern Alps, Italy), Uranium, 2, 215–240, 1986.
Carraro, F. and Ferrara, G.: Alpine “Tonalite” at Miagliano, Biella (Zona Diorito-Kinzigitica). A preliminary note, Schweiz. Miner. Petrog., 48, 75–80, 1968.
Carslaw, H. and Jaeger, J.: Conduction of Heat in Solids, Clarendon Press, Oxford, United Kingdom, 510 pp., ISBN-10: 0198533683, 1959.
Casati, P.: Tettonismo e sedimentazione nel settore occidentale delle Alpi Meridionali durante il tardo Paleozoico, il Triassico e il Giurassico, Riv. Ital. Paleontologia Stratigrafia, 84, 313–326, 1978.
Cassinis, G., Perotti, C. R., and Ronchi, A.: Permian continental basins in the Southern Alps (Italy) and peri-mediterranean correlations, Int. J. Earth Sci., 101, 129–157, https://doi.org/10.1007/s00531-011-0642-6, 2012.
Cassinis, G., Perotti, C., and Santi, G.: Post-Variscan Verrucano-like deposits in Italy, and the onset of the alpine tectono-sedimentary cycle, Earth-Sci. Rev., 185, 476–497, 2018.
Castellarin, A., Lucchini, F., Rossi, P. L., Selli, L., and Simboli, G.: The Middle Triassic magmatic-tectonic arc development in the Southern Alps, Tectonophysics, 146, 79–89, 1988.
Colombo, M., Di Capua, A., Livio, F., Scaramuzzo, E., and Tringali, G.: Volcanic and tectonic interaction during the Permian geodynamic event: new insights from the Lugano-Varese district, Southern Alps, (Italy-Switzerland), EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-16466, https://doi.org/10.5194/egusphere-egu25-16466, 2025.
De Min, A., Velicogna, M., Ziberna, L., Chiaradia, M., Alberti, A., and Marzoli, A.: Triassic magmatism in the European Southern Alps as an early phase of Pangea break-up, Geol. Mag., 157, 1800–1822, https://doi.org/10.1017/S0016756820000084, 2020.
Di Battistini, G., Bargossi, G. M., Spotti, G., and Toscani, L.: Andesites of the late Hercynian volcanic sequence in Trentino Alto Adige (Northen Italy), Rendiconti Società Italiana Mineralogia Petrologia, 43, 1087–1100, 1988.
Diella, V., Spalla, M. I., and Tunesi, A.: Contrasting thermomechanical evolutions in the Southalpine metamorphic basement of the Orobic Alps (Central Alps, Italy), J. Metamorph. Geol., 10, 203–219, https://doi.org/10.1111/j.1525-1314.1992.tb00079.x, 1992.
Di Paola, S., Spalla, M. I., and Gosso, G.: New structural mapping and metamorphic evolution of the Domaso Cortafo Zone (Southern Alps-Lake Como), Memorie di Scienze Geologiche, Padova, 53, 1–14, 2001.
Doglioni, C.: Geological remarks on the relationships between extension and convergent geodynamic settings, Tectonophysics, 252, 253–267, https://doi.org/10.1016/0040-1951(95)00087-9, 1995.
Ehlers, T. A., Willett, S. D., Armstrong, P. A., and Chapman, D. S.: Exhumation of the central Wasatch Mountains, Utah: 2. Thermokinematic model of exhumation, erosion, and thermochronometer interpretation, J. Geophys. Res.-Sol. Ea., 108, 2173, https://doi.org/10.1029/2001JB001723, 2003.
Elter, F. M., Gaggero, L., Mantovani, F., Pandeli, E., and Costamagna, L. G.: The Atlas-East Variscan-Elbe shear system and its role in the formation of the pull-apart Late Palaeozoic basins, Int. J. Earth Sci., 109, 739–760, https://doi.org/10.1007/s00531-020-01830-y, 2020.
Ferrando, S., Bernoulli, D., and Compagnoni, R.: The Canavese zone (internal Western Alps): a distal margin of Adria, Schweiz. Miner. Petrog., 84, 237–259, 2004.
Finger, F. and Steyrer, H. P.: I-type granitoids as indicators of a late Paleozoic convergent ocean–continent margin along the southern flank of the central European Variscan orogen, Geology, 18, 1207–1210, 1990.
Finger, F. and Steyrer, H. P.: Comments and Replies on I-type granitoids as indicators of a late Paleozoic convergent ocean–continent margin along the southern flank of the central European Variscan orogen, Geology, 19, 1245–1248, 1991.
Furrer, H.: The Kalkschieferzone (Upper Meride Limestone; Ladinian) near Meride (Canton Ticino, Southern Switzerland) and the evolution of a Middle Triassic intraplatform basin, Eclogae Geol. Helv., 88, 827–852, 1995.
Gaetani, M.: From Permian to Cretaceous: Adria as pivotal between extensions and rotations of Tethys and Atlantic Oceans, Journal of the Virtual Explorer, 36, 3–46, https://doi.org/10.3809/jvirtex.2010.00235, 2010.
Gaetani, M., Gnaccolini, M., Jadoul, F., and Garzanti, E.: Multiorder sequence stratigraphy in the Triassic system of the western Southern Alps: Mesozoic and Cenozoic sequence stratigraphy of European basins, SEPM Special Publications, 60, 701–717, 1998.
Gautheron, C., Tassan-Got, L., Barbarand, J., and Pagel, M.: Effect of alpha-damage annealing on apatite
Giger, M.: Geochronologische und petrographische Studien an Geröllen und Sedimenten der Gonfolite Lombarda Gruppe (Südschweiz und Norditalien) und ihr Vergleich mit dem alpinen Hinterland, PhD thesis, University of Bern, Bern, Switzerland, 227 pp., 1991.
Giorno, M., Barale, L., Bertok, C., Frenzel, M., Looser, N., Guillong, M., Bernasconi, S., and Martire, L.: Sulfide-associated hydrothermal dolomite and calcite reveal a shallow burial depth for Alpine-type Zn-(Pb) deposits, Geology, 50, 853–858, https://doi.org/10.1130/G49812.1, 2022.
Govi, M: Geologia del territorio compreso tra il Lago di Lugano e la Val Marchirolo, Studi e Ricerche della Divisione Geomineraria del CNR, 3, 160–217, 1960.
Gretter, N., Ronchi, A., Langone, A., and Perotti, C. R.: The transition between the two major Permian tectono-stratigraphic cycles in the central Southern Alps: results from facies analysis and U/Pb geochronology, Int. J. Earth Sci., 102, 1181–1202, https://doi.org/10.1007/s00531-013-0886-4, 2013.
Handy, M. R., Franz, L., Heller, F., Janott, B., and Zurbriggen, R.: Multistage accretion and exhumation of the continental crust (Ivrea crustal section, Italy and Switzerland), Tectonics, 18, 1154–1177, https://doi.org/10.1029/1999TC900034, 1999.
Heberer, B., Reverman, R. L., Fellin, M. G., Neubauer, F., Dunkl, I., Zattin, M., Seward, D., Genser, J., and Brack, P.: Postcollisional cooling history of the Eastern and Southern Alps and its linkage to Adria indentation, Int. J. Earth Sci., 106, 1557–1580, https://doi.org/10.1007/s00531-016-1367-3, 2016.
Hourigan, J. K., Reiners, P. W., and Brandon, M. T.: U–Th zonation-dependent alpha-ejection in
Hunziker, J. C.: Rb–Sr and K–Ar age determination and the Alpine tectonic history of the Western Alps, Mem. Ist. Geol. Mineral. Univ. Padova, 31, 5–55, 1974.
Hurford, A. J.: Cooling and uplift patterns in the Lepontine Alps South Central Switzerland and an age of vertical movement on the Insubric fault line, Contrib. Mineral. Petr., 92, 413–427, 1986.
Jäger, E. and Faul, H.: Altersbestimmungen an einigen Schweizer Gesteinen und dem Granit von Baveno, Schweiz. Miner. Petrog., 40, 10–12, 1960.
Jongmans, W. J. and Ritter, E.: Die Karbonflora der Schweiz, Beiträge zur geologischen Karte der Schweiz, Kümmerly und Frey, 116 pp., 1960.
Kalin, O. and Trümpy, D.: Sedimentation und Palaotektonik in den westlichen Sudalpen: Zur triasisch-jurassischen Geschichte des Monte Nudo-Beckens, Eclogae Geol. Helv., 70, 295–350, 1960.
Karakas, O., Wotzlaw, J. F., Guillong, M., Ulmer, P., Brack, P., Economos, R., Bergantzm G. W., Sinigoi, S., and Bachmann, O.: The pace of crustal-scale magma accretion and differentiation beneath silicic caldera volcanoes, Geology, 47, 719–723, https://doi.org/10.1130/G46020.1, 2019.
Ketcham, R. A., Gautheron, C., and Tassan-Got, L.: Accounting for long alpha-particle stopping distances in (U–Th–Sm)
Locchi, S., Zanchetta, S., and Zanchi, A.: Evidence of Early Permian extension during the post-Variscan evolution of the central Southern Alps (N Italy), Int. J. Earth Sci., 111, 1717–1738, https://doi.org/10.1007/s00531-022-02220-2, 2022.
Lorenz, V. and Nicholls, I. A.: Plate and intraplate processes of Hercynian Europe during the Late Paleozoic, Tectonophysics, 107, 25–56, 1984.
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.
Marocchi, M., Morelli, C., Mair, V., Klötzli, U., and Bargossi, G. M.: Evolution of Large Silicic Magma Systems: New U–Pb Zircon Data on the NW Permian Athesian Volcanic Group (Southern Alps, Italy), J. Geol., 116, 480–498, 2008.
Marrett, R. and Allmendinger, R. W.: Kinematic analysis of fault-slip data, J. Struct. Geol., 12, 973–986, 1990.
Martin, S., Bigazzi, G., Zattin, M., Viola, G., and Balestrieri, M. L.: Neogene kinematics of the Giudicarie fault (Central-Eastern Alps, Italy): new apatite fission-track data, Terra Nova, 10, 217–221, 1998.
Martin, S., Toffolo, L., Moroni, M., Montorfano, C., Secco, L., Agnini, C., Nimis, P., and Tumiati, S.: Siderite deposits in northern Italy: Early Permian to Early Triassic hydrothermalism in the Southern Alps, Lithos, 284–285, 276–295, https://doi.org/10.1016/j.lithos.2017.04.002, 2017.
McDowell, F. W.: Potassium-argon ages from the Ceneri zone, Southern Swiss Alps, Contrib. Mineral. Petr., 28, 165–182, 1970.
McDowell, F. W. and Schmid, R.: Potassium-argon ages from the Valle d'Ossola section of the Ivrea-Verbano zone (northern Italy), Schweiz. Miner. Petrog., 48, 205–210, 1968.
Mohn, G., Manatschal, G., Müntener, O., Beltrando, M., and Masini, E.: Unravelling the interaction between tectonic and sedimentary processes during lithospheric thinning in the Alpine Tethys margins, Int. J. Earth Sci., 99, 75–101, 2010.
Mohn, G., Manatschal, G., Masini, E., and Müntener, O.: Rift-related inheritance in orogens: a case study from the Austroalpine nappes in Central Alps (SE-Switzerland and N-Italy), Int. J. Earth Sci., 100, 937–961, 2011.
Mohn, G., Manatschal, G., Beltrando, M., Masini, E., and Kusznir, N.: Necking of continental crust in magma-poor rifted margins: Evidence from the fossil Alpine Tethys margins, Tectonics, 31, TC1012, https://doi.org/10.1029/2011TC002961, 2012.
Molli, G., Brogi, A., Caggianelli, A., Capezzuoli, E., Liotta, D., Spina, A., and Zibra, I. Late Palaeozoic tectonics in Central Mediterranean: a reappraisal, Swiss J. Geosci., 113, 23, https://doi.org/10.1186/s00015-020-00375-1. 2020.
Muttoni, G., Kent, D. V., Garzanti, E., Brack, P., Abrahamsen, N., and Gaetani, M.: Early Permian Pangea `B'to Late Permian Pangea “A”, Earth Planet. Sc. Lett., 215, 379–394, https://doi.org/10.1016/S0012-821X(03)00452-7, 2003.
Muttoni, G., Gaetani, M., Kent, D. V., Sciunnach, D., Angiolini, L., Berra, F., Garzanti, E., Mattei, M., and Zanchi, A.: Opening of the Neo-Tethys Ocean and the Pangea B to Pangea A transformation during the Permian, GeoArabia, 14, 17–48, https://doi.org/10.2113/geoarabia140417, 2009.
Naliboff, J. B., Buiter, S. J., Péron-Pinvidic, G., Osmundsen, P. T., and Tetreault, J.: Complex fault interaction controls continental rifting, Nat. Commun., 8, 1179, https://doi.org/10.1038/s41467-017-00904-x, 2017.
Peron-Pinvidic, G., Manatschal, G., and Osmundsen, P. T.: Structural comparison of archetypal Atlantic rifted margins: A review of observations and concepts, Mar. Petrol. Geol., 43, 21–47, https://doi.org/10.1016/j.marpetgeo.2013.02.002, 2013.
Pohl, F., Froitzheim, N., Obermüller, G., Tomaschek, F., Schröder, O., Nagel, T. J., Schiunnach, D., and Heuser, A.: Kinematics and age of syn-intrusive detachment faulting in the Southern Alps: Evidence for Early Permian crustal extension and implications for the Pangea A versus B Controversy, Tectonics, 37, 3668–3689, https://doi.org/10.1029/2018TC004974, 2018,
Pomella, H., Stipp, M., and Fügenschuh, B.: Thermochronological record of thrusting and strike-slip faulting along the Giudicarie fault system (Alps, Northern Italy), Tectonophysics, 579, 118–130, https://doi.org/10.1016/J.Tecto.2012.04.015, 2012.
QGIS Association: QGIS Geographic Information System, QGIS Association [code and data set], https://qgis.org/it/site/, last access: 3 April 2024.
Quick, J. E., Sinigoi, S., Peressini, G., Demarchi, G., Wooden, J. L., and Sbisà, A.: Magmatic plumbing of a large Permian caldera exposed to a depth of 25 km, Geology, 37, 603–606, 2009.
Real, C., Fassmer, K., Carosi, R., Froitzheim, N., Rubatto, D., Groppo, C., Münker. C., and Ferrando, S.: Carboniferous–Triassic tectonic and thermal evolution of the middle crust section of the Dervio–Olgiasca Zone (Southern Alps), J. Metamorph. Geol., 41, 685–718, https://doi.org/10.1111/jmg.12714, 2023.
Reiners, P. W. and Brandon, M. T.: Using thermochronology to understand orogenic erosion, Annu. Rev. Earth Pl. Sc., 34, 419–466, https://doi.org/10.1146/annurev.earth.34.031405.125202, 2006.
Reiners, P. W., Spell, T. L., Nicolescu, S., and Zanetti, K. A.: Zircon
Renesto, S. and Stockar, R.: First record of a coelacanth fish from the Middle Triassic Meride Limestone of Monte San Giorgio (Canton Ticino, Switzerland), Riv. Ital. Paleontol. S., 124, 639–653, 2018.
Reverman, R. L., Fellin, M. G., Herman, F., Willett, S. D., and Fitoussi, C.: Climatically versus tectonically forced erosion in the Alps: Thermochronometric constraints from the Adamello Complex, Southern Alps, Italy, Earth Planet. Sc. Lett., 339, 127–138, https://doi.org/10.1016/j.epsl.2012.04.051, 2012.
Roda, M., Regorda, A., Spalla, M. I., and Marotta, A. M.: What drives Alpine Tethys opening? Clues from the review of geological data and model predictions, Geol. J., 54, 2646–2664, https://doi.org/10.1002/gj.3316, 2019.
Rosenberg, C. L. and Kissling, E.: Three-dimensional insight into Central-Alpine collision: Lower-plate or upper-plate indentation?, Geology, 41, 1219–1222, https://doi.org/10.1130/G34584.1, 2013.
Scaramuzzo, E., Livio, F. A., Granado, P., Di Capua, A., and Bitonte, R.: Anatomy and kinematic evolution of an ancient passive margin involved into an orogenic wedge (Western Southern Alps, Varese area, Italy and Switzerland), Swiss J. Geosci., 115, 4, https://doi.org/10.1186/s00015-021-00404-7, 2022.
Schaltegger, U. and Brack, P.: Crustal-scale magmatic systems during intracontinental strike-slip tectonics: U, Pb and Hf isotopic constraints from Permian magmatic rocks of the Southern Alps, Int. J. Earth Sci., 96, 1131–1151, https://doi.org/10.1007/s00531-006-0165-8, 2007.
Shuster, D. L., Flowers, R. M., and Farley, K. A.: The influence of natural radiation damage on helium diffusion kinetics in apatite, Earth Planet. Sc. Lett., 249, 148–161, https://doi.org/10.1016/j.gca.2008.10.013, 2006.
Siegesmund, S., Layer, P., Dunkl, I., Vollbrecht, A., Steenken, A., Wemmer, K., and Ahrendt, H.: Exhumation and deformation history of the lower crustal section of the Valstrona di Omegna in the Ivrea Zone, southern Alps, Geological Society, London, Special Publications, 298, 45–68, https://doi.org/10.1144/SP298.3, 2008.
Siletto, G. B., Spalla, M. I., Tunesi, A., Lardeaux, J. M., and Colombo, A.: Pre-Alpine structural and metamorphic histories in the Orobic Southern Alps, Italy, in: Pre-Mesozoic geology in the Alps, edited by: Von Raumer, J. F. and Neubauer, F., Springer, Berlin, Germany, 585–598, ISBN-10: 3642846424, 1993.
Spalla, M. I., Diella, V., Pigazzini, N.., Siletto, G. B., and Gosso, G.: Significato tettonico della transizione Cld-And nelle metapeliti del Basamento Sudalpino (Alta Val Camonica), Rendiconti della Società Geologica Italiana, 2, 182–183, 2006.
Stampfli, G. M.: The Intra-Alpine terrain: a Paleotethyan remnant in the Alpine Variscides, Eclogae Geol. Helv., 89, 13–42, 1996.
Stampfli, G. M.: Tethyan oceans, in: Tectonics and Magmatism in Turkey and Surrounding Area, edited by: Bozkurt, E., Winchester, J. A., and Piper, J. D. A., Geological Society, London, Special Publications, 173, 1–23, ISBN 1-86239-064-9, 2000.
Stampfli, G. M. and Kozur, H. W.: Europe from the Variscan to the Alpine cycles, in: European Lithosphere Dynamics, edited by: Gee, D. G. and Stephenson, R. A., Geological Society, London, Memoirs, 32, 57–82, https://doi.org/10.1144/GSL.MEM.2006.032.01.04, 2006.
Stille, P. and Buletti, M.: Nd-Sr isotopic characteristics of the Lugano volcanic rocks and constraints on the continental crust formation in the South Alpine domain (N-Italy-Switzerland), Contrib. Mineral. Petr., 96, 140–150, 1987.
Stockar, R.: Facies, depositional environment, and palaeoecology of the Middle Triassic Cassina beds (Meride Limestone, Monte San Giorgio, Switzerland), Swiss J. Geosci., 103, 101–119, https://doi.org/10.1007/s00015-010-0008-2, 2010.
Stockar, R., Adatte, T., Baumgartner, P. O., and Föllmi, K. B.: Palaeoenvironmental significance of organic facies and stable isotope signatures: the Ladinian San Giorgio Dolomite and Meride Limestone of Monte San Giorgio (Switzerland, WHL UNESCO), Sedimentology, 60, 239–269, https://doi.org/10.1111/sed.12021, 2013.
Storck, J. C., Brack, P., Wotzlaw, J. F., and Ulmer, P.: Timing and evolution of Middle Triassic magmatism in the Southern Alps (northern Italy), J. Geol. Soc. London, 176, 253–268, 2019.
Torsvik, T. H. and Cocks, L. R. M.: Earth geography from 400 to 250 Ma: a palaeomagnetic, faunal and facies review, J. Geol. Soc. London, 161, 555–572, 2004.
Visonà, D.: Plutonismo basico ercinico nel Sudalpino delle Alpi Orientali: primi dati per un modello di tettonica a placche ercinica, Rendiconti della Società geologica italiana, 5, 105–107, https://doi.org/10.1007/s005310100200, 1982.
Von Raumer, J., Stampfli, G., Borel, G., and Bussy, F.: Organization of pre-Variscan basement areas at the north-Gondwanan margin, Int. J. Earth Sci., 91, 35–52, 2002.
Welch, B. L.: The generalization of “Student's” problem when several different population variances are involved, Biometrika, 34, 28–35, 1947.
Willett, S. D., Herman, F., Fox, M., Stalder, N., Ehlers, T. A., Jiao, R., and Yang, R.: Bias and error in modelling thermochronometric data: resolving a potential increase in Plio-Pleistocene erosion rate, Earth Surf. Dynam., 9, 1153–1221, https://doi.org/10.5194/esurf-9-1153-2021, 2021.
Wilson, J. T.: Static or mobile earth: the current scientific revolution, P. Am. Philos. Soc., 112, 309–320, 1968.
Wilson, R. W., Houseman, G. A., Buiter, S. J. H., McCaffrey, K. J., and Doré, A. G.: Fifty years of the Wilson Cycle concept in plate tectonics: an overview, Geological Society, London, Special Publications, 470, 1–17, https://doi.org/10.1144/SP470-2019-58, 2019.
Winterer, E. L. and Bosellini, A.: Subsidence and sedimentation on Jurassic passive continental margin, Southern Alps, Italy, AAPG Bull., 65, 394–421, https://doi.org/10.1306/2F9197E2-16CE-11D7-8645000102C1865D, 1981.
Withjack, M. O., Islam, Q. T., and La Pointe, P. R.: Normal faults and their hanging-wall deformation: an experimental study, AAPG Bull., 79, 1–17, https://doi.org/10.1306/8D2B1494-171E-11D7-8645000102C1865D, 1995.
Wolff, R., Dunkl, I., Kiesselbach, G., Wemmer, K., and Siegesmund, S.: Thermochronological constraints on the multiphase exhumation history of the Ivrea-Verbano Zone of the Southern Alps, Tectonophysics, 579, 104–117, https://doi.org/10.1016/j.tecto.2012.03.019, 2012.
Zanchetta, S., D'Adda, P., Zanchi, A., Barberini, V., and Villa, I. M.: Cretaceous-Eocene compression in the central Southern Alps (N Italy) inferred from
Zanchetta, S., Malusà, M. G., and Zanchi, A.: Precollisional development and Cenozoic evolution of the Southalpine retrobelt (European Alps), Lithosphere, 7, 662–681, https://doi.org/10.1130/L466.1, 2015.
Zanchi, A., Zanchetta, S., Berio, L., Berra, F., and Felletti, F.: Low-angle normal faults record Early Permian extensional tectonics in the Orobic Basin (Southern Alps, N Italy), Ital. J. Geosci., 138, 184–201, https://doi.org/10.3301/IJG.2018.35, 2019.
Zanetti, A., Mazzucchelli, M., Sinigoi, S., Giovanardi, T., Peressini, G., and Fanning, M.: SHRIMP U–Pb zircon Triassic intrusion age of the Finero mafic complex (Ivrea–Verbano Zone, Western Alps) and its geodynamic implications, J. Petrol., 54, 2235–2265, 2013.
Zanoni, D. and Spalla, M. I.: The Variscan evolution in the basement cobbles of the Permian Ponteranica Formation by microstructural and petrologic analysis, Ital. J. Geosci., 137, 254–271, https://doi.org/10.3301/IJG.2018.12, 2018.
Zattin, M., Cuman, A., Fantoni, R., Martin, S., Scotti, P., and Stefani, C.: From Middle Jurassic heating to Neogene cooling: The thermochronological evolution of the southern Alps, Tectonophysics, 414, 191–202, https://doi.org/10.1016/J.Tecto.2005.10.020, 2006.
Ziegler, P. A. and Stampfli, G. M.: Late Paleozoic-Early Mesozoic plate boundary reorganization: collapse of the Variscan orogen and opening of Neotethys, in: Permian continental deposits of Europe and other areas. Regional reports and correlations, edited by: Cassinis, G., Monografie di Natura Bresciana, Grafo, Brescia, Italy, 17–34, 2001.
Zingg, A., Handy, M. R., Hunziker, J. C., and Schmid, S. M.: Tectonometamorphic history of the Ivrea Zone and its relationship to the crustal evolution of the Southern Alps, Tectonophysics, 182, 169–192, https://doi.org/10.1016/0040-1951(90)90349-D, 1990.
Zorn, H.: Paläontologische, stratigraphische und sedimentologische Untersuchungen des Salvatoredolomits (Mitteltrias) der Tessiner Kalkalpen: unter besonderer Berücksichtigung der Mikrofazies, Diagenese und Taxionomie der Lamellibranchiata, Schweiz. Paläontol. Abh., 91, 1–90, 1971.
Zwingmann, H. and Mancktelow, N.: Timing of Alpine fault gouges, Earth Planet. Sc. Lett., 223, 415–425, https://doi.org/10.1016/j.epsl.2004.04.041, 2004.
Executive editor
I concur with the AE's assessment that this paper presents valuable new models on the Permo-Triassic evolution of the Alps.
I concur with the AE's assessment that this paper presents valuable new models on the...
Short summary
We address the transition between the Paleozoic Variscan and Alpine Mesozoic–Cenozoic cycles using tectono-stratigraphy and thermochronology. This transition unfolds through a multi-phase rifting history. An initial rifting stage occurred in the early Permian, followed in the early–middle Permian by a phase of transcurrent tectonics. This was succeeded by a period of erosion/non-deposition in the middle Permian. Crustal stretching in the Middle Triassic marked the onset of the Alpine cycle.
We address the transition between the Paleozoic Variscan and Alpine Mesozoic–Cenozoic cycles...
