Articles | Volume 4, issue 2
https://doi.org/10.5194/se-4-423-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/se-4-423-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
11 Nov 2013
Research article |
| 11 Nov 2013
Experimental deformation and recrystallization of olivine – processes and timescales of damage healing during postseismic relaxation at mantle depths
C. A. Trepmann
Department for Earth and Environmental Sciences, Ludwig-Maximilians-Universität München, Germany
J. Renner
Institute for Geology, Mineralogy, and Geophysics, Ruhr-Universität Bochum, Germany
A. Druiventak
Institute for Geology, Mineralogy, and Geophysics, Ruhr-Universität Bochum, Germany
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Eur. J. Mineral., 32, 521–544, https://doi.org/10.5194/ejm-32-521-2020, https://doi.org/10.5194/ejm-32-521-2020, 2020
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We analysed apatite–allanite/epidote coronae around monazite and xenotime in deformed Permian pegmatites from the Austroalpine basement. Microscopy, chemical analysis and EBSD showed that these coronae formed by dissolution–precipitation processes during deformation of the host rocks. Dating of monazite and xenotime confirmed the magmatic origin of the corona cores, while LA-ICP-MS dating of allanite established a date of ~ 60 Ma for corona formation and deformation in the Austroalpine basement.
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We used microscopy and electron backscatter diffraction to analyse the deformation behaviour of feldspar at greenschist facies conditions in mylonitic pegmatites of the Austroalpine basement. There are strong uncertainties about feldspar deformation, mainly because of the varying contributions of different deformation processes. We observed that deformation is mainly the result of coupled fracturing and dislocation glide, followed by growth and granular flow.
J. Bial and C. A. Trepmann
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Solid Earth, 4, 263–276, https://doi.org/10.5194/se-4-263-2013, https://doi.org/10.5194/se-4-263-2013, 2013
Olaf Kolditz, Christopher McDermott, Jeoung Seok Yoon, Jörg Renner, Li Zhuang, Andrew Fraser-Harris, Michael Chandler, Samuel Graham, Ju Wang, and Mostafa Mollaali
Saf. Nucl. Waste Disposal Discuss., https://doi.org/10.5194/sand-2024-2, https://doi.org/10.5194/sand-2024-2, 2024
Revised manuscript under review for SaND
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The DECOVALEX Task SAFENET is dedicated to advancing the understanding of fracture nucleation and evolution processes in crystalline rocks, with applications in nuclear waste management and geothermal reservoir engineering.
Felix Hentschel, Emilie Janots, Claudia A. Trepmann, Valerie Magnin, and Pierre Lanari
Eur. J. Mineral., 32, 521–544, https://doi.org/10.5194/ejm-32-521-2020, https://doi.org/10.5194/ejm-32-521-2020, 2020
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We analysed apatite–allanite/epidote coronae around monazite and xenotime in deformed Permian pegmatites from the Austroalpine basement. Microscopy, chemical analysis and EBSD showed that these coronae formed by dissolution–precipitation processes during deformation of the host rocks. Dating of monazite and xenotime confirmed the magmatic origin of the corona cores, while LA-ICP-MS dating of allanite established a date of ~ 60 Ma for corona formation and deformation in the Austroalpine basement.
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The technique of X-ray computed tomography (CT) is widely used in multiple disciplines such as medicine, industry and earth sciences. However, quantitative analysis from the reconstructed images are subject to errors due to technical limitations and subsequent evaluation workflows. The paper addresses the uncertainties related to the estimation of porosity from these images and compares the results with laboratory measurements. Accurate porosity estimates are linked to sufficient resolution.
Felix Hentschel, Claudia A. Trepmann, and Emilie Janots
Solid Earth, 10, 95–116, https://doi.org/10.5194/se-10-95-2019, https://doi.org/10.5194/se-10-95-2019, 2019
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We used microscopy and electron backscatter diffraction to analyse the deformation behaviour of feldspar at greenschist facies conditions in mylonitic pegmatites of the Austroalpine basement. There are strong uncertainties about feldspar deformation, mainly because of the varying contributions of different deformation processes. We observed that deformation is mainly the result of coupled fracturing and dislocation glide, followed by growth and granular flow.
K. Klevakina, J. Renner, N. Doltsinis, and W. Adeagbo
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A. E. Ortiz R., R. Jung, and J. Renner
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Stress along a subduction plate boundary is important for understanding subduction phenomena such as earthquakes. We estimated paleo-stress using quartz recrystallized grain size combined with deformation temperature and P–T paths of exhumed rocks. The obtained results show differential stresses of 30.8–82.7 MPa consistent over depths of 17–27 km in the paleo-subduction boundary. The obtained stress may represent the initial conditions under which slow earthquakes nucleated in the same domain.
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Adam J. Cawood, Hannah Watkins, Clare E. Bond, Marian J. Warren, and Mark A. Cooper
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Johanna Heeb, David Healy, Nicholas E. Timms, and Enrique Gomez-Rivas
Solid Earth, 14, 985–1003, https://doi.org/10.5194/se-14-985-2023, https://doi.org/10.5194/se-14-985-2023, 2023
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Hydration of rocks is a key process in the Earth’s crust and mantle that is accompanied by changes in physical traits and mechanical behaviour of rocks. This study assesses the influence of stress on hydration reaction kinetics and mechanics in experiments on anhydrite. We show that hydration occurs readily under stress and results in localized hydration along fractures and mechanic weakening. New gypsum growth is selective and depends on the stress field and host anhydrite crystal orientation.
Roy Helge Gabrielsen, Panagiotis Athanasios Giannenas, Dimitrios Sokoutis, Ernst Willingshofer, Muhammad Hassaan, and Jan Inge Faleide
Solid Earth, 14, 961–983, https://doi.org/10.5194/se-14-961-2023, https://doi.org/10.5194/se-14-961-2023, 2023
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The Barents Shear Margin defines the border between the relatively shallow Barents Sea that is situated on a continental plate and the deep ocean. This margin's evolution history was probably influenced by plate tectonic reorganizations. From scaled experiments, we deduced several types of structures (faults, folds, and sedimentary basins) that help us to improve the understanding of the history of the opening of the North Atlantic.
Leslie Logan, Ervin Veress, Joel B. H. Andersson, Olof Martinsson, and Tobias E. Bauer
Solid Earth, 14, 763–784, https://doi.org/10.5194/se-14-763-2023, https://doi.org/10.5194/se-14-763-2023, 2023
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The Pahtohavare Cu ± Au deposits in the Kiruna mining district have a dubious timing of formation and have not been contextualized within an up-to-date tectonic framework. Structural mapping was carried out to reveal that the deposits are hosted in brittle structures that cut a noncylindrical, SE-plunging anticline constrained to have formed during the late-Svecokarelian orogeny. These results show that Cu ± Au mineralization formed more than ca. 80 Myr after iron oxide–apatite mineralization.
Alexandra Tamas, Dan M. Tamas, Gabor Tari, Csaba Krezsek, Alexandru Lapadat, and Zsolt Schleder
Solid Earth, 14, 741–761, https://doi.org/10.5194/se-14-741-2023, https://doi.org/10.5194/se-14-741-2023, 2023
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Tectonic processes are complex and often difficult to understand due to the limitations of surface or subsurface data. One such process is inversion tectonics, which means that an area initially developed in an extension (such as the opening of an ocean) is reversed to compression (the process leading to mountain building). In this research, we use a laboratory method (analogue modelling), and with the help of a sandbox, we try to better understand structures (folds/faults) related to inversion.
Elizabeth Parker Wilson, Pablo Granado, Pablo Santolaria, Oriol Ferrer, and Josep Anton Muñoz
Solid Earth, 14, 709–739, https://doi.org/10.5194/se-14-709-2023, https://doi.org/10.5194/se-14-709-2023, 2023
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This work focuses on the control of accommodation zones on extensional and subsequent inversion in salt-detached domains using sandbox analogue models. During extension, the transfer zone acts as a pathway for the movement of salt, changing the expected geometries. When inverted, the salt layer and syn-inversion sedimentation control the deformation style in the salt-detached cover system. Three natural cases are compared to the model results and show similar inversion geometries.
Oriol Ferrer, Eloi Carola, and Ken McClay
Solid Earth, 14, 571–589, https://doi.org/10.5194/se-14-571-2023, https://doi.org/10.5194/se-14-571-2023, 2023
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Using an experimental approach based on scaled sandbox models, this work aims to understand how salt above different rotational fault blocks influences the cover geometry and evolution, first during extension and then during inversion. The results show that inherited salt structures constrain contractional deformation. We show for the first time how welds and fault welds are reopened during contractional deformation, having direct implications for the subsurface exploration of natural resources.
Chiara Montemagni, Stefano Zanchetta, Martina Rocca, Igor M. Villa, Corrado Morelli, Volkmar Mair, and Andrea Zanchi
Solid Earth, 14, 551–570, https://doi.org/10.5194/se-14-551-2023, https://doi.org/10.5194/se-14-551-2023, 2023
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The Vinschgau Shear Zone (VSZ) is one of the largest and most significant shear zones developed within the Late Cretaceous thrust stack in the Austroalpine domain of the eastern Alps. 40Ar / 39Ar geochronology constrains the activity of the VSZ between 97 and 80 Ma. The decreasing vorticity towards the core of the shear zone, coupled with the younging of mylonites, points to a shear thinning behavior. The deepest units of the Eo-Alpine orogenic wedge were exhumed along the VSZ.
Jordi Miró, Oriol Ferrer, Josep Anton Muñoz, and Gianreto Manastchal
Solid Earth, 14, 425–445, https://doi.org/10.5194/se-14-425-2023, https://doi.org/10.5194/se-14-425-2023, 2023
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Using the Asturian–Basque–Cantabrian system and analogue (sandbox) models, this work focuses on the linkage between basement-controlled and salt-decoupled domains and how deformation is accommodated between the two during extension and subsequent inversion. Analogue models show significant structural variability in the transitional domain, with oblique structures that can be strongly modified by syn-contractional sedimentation. Experimental results are consistent with the case study.
Junichi Fukuda, Takamoto Okudaira, and Yukiko Ohtomo
Solid Earth, 14, 409–424, https://doi.org/10.5194/se-14-409-2023, https://doi.org/10.5194/se-14-409-2023, 2023
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We measured water distributions in deformed quartz by infrared spectroscopy mapping and used the results to discuss changes in water distribution resulting from textural development. Because of the grain size reduction process (dynamic recrystallization), water contents decrease from 40–1750 wt ppm in host grains of ~2 mm to 100–510 wt ppm in recrystallized regions composed of fine grains of ~10 µm. Our results indicate that water is released and homogenized by dynamic recrystallization.
Bastien Walter, Yves Géraud, Alexiane Favier, Nadjib Chibati, and Marc Diraison
EGUsphere, https://doi.org/10.5194/egusphere-2023-397, https://doi.org/10.5194/egusphere-2023-397, 2023
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Lake Abhe in southwestern Djibouti is known for its exposures of massive hydrothermal chimneys and hot springs on the lake’s eastern shore. This study highlights the control of the main structural faults of the area on the development of these hydrothermal features. This work contributes to better understand hydrothermal fluid pathways in this area and may help further exploration for the geothermal development of this remarkable site.
Michael Rudolf, Matthias Rosenau, and Onno Oncken
Solid Earth, 14, 311–331, https://doi.org/10.5194/se-14-311-2023, https://doi.org/10.5194/se-14-311-2023, 2023
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Analogue models of tectonic processes rely on the reproduction of their geometry, kinematics and dynamics. An important property is fault behaviour, which is linked to the frictional characteristics of the fault gouge. This is represented by granular materials, such as quartz sand. In our study we investigate the time-dependent frictional properties of various analogue materials and highlight their impact on the suitability of these materials for analogue models focusing on fault reactivation.
Jessica Barabasch, Joyce Schmatz, Jop Klaver, Alexander Schwedt, and Janos L. Urai
Solid Earth, 14, 271–291, https://doi.org/10.5194/se-14-271-2023, https://doi.org/10.5194/se-14-271-2023, 2023
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We analysed Zechstein salt with microscopes and observed specific microstructures that indicate much faster deformation in rock salt with fine halite grains when compared to salt with larger grains. This is important because people build large cavities in the subsurface salt for energy storage or want to deposit radioactive waste inside it. When engineers and scientists use grain-size data and equations that include this mechanism, it will help to make better predictions in geological models.
Nicolás Molnar and Susanne Buiter
Solid Earth, 14, 213–235, https://doi.org/10.5194/se-14-213-2023, https://doi.org/10.5194/se-14-213-2023, 2023
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Progression of orogenic wedges over pre-existing extensional structures is common in nature, but deciphering the spatio-temporal evolution of deformation from the geological record remains challenging. Our laboratory experiments provide insights on how horizontal stresses are transferred across a heterogeneous crust, constrain which pre-shortening conditions can either favour or hinder the reactivatation of extensional structures, and explain what implications they have on critical taper theory.
Tania Habel, Martine Simoes, Robin Lacassin, Daniel Carrizo, and German Aguilar
Solid Earth, 14, 17–42, https://doi.org/10.5194/se-14-17-2023, https://doi.org/10.5194/se-14-17-2023, 2023
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The Central Andes are one of the most emblematic reliefs on Earth, but their western flank remains understudied. Here we explore two rare key sites in the hostile conditions of the Atacama desert to build cross-sections, quantify crustal shortening, and discuss the timing of this deformation at ∼20–22°S. We propose that the structures of the Western Andes accommodated significant crustal shortening here, but only during the earliest stages of mountain building.
Naïm Célini, Frédéric Mouthereau, Abdeltif Lahfid, Claude Gout, and Jean-Paul Callot
Solid Earth, 14, 1–16, https://doi.org/10.5194/se-14-1-2023, https://doi.org/10.5194/se-14-1-2023, 2023
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We investigate the peak temperature of sedimentary rocks of the SW Alps (France), using Raman spectroscopy on carbonaceous material. This method provides an estimate of the peak temperature achieved by organic-rich rocks. To determine the timing and the tectonic context of the origin of these temperatures we use 1D thermal modelling. We find that the high temperatures up to 300 °C were achieved during precollisional extensional events, not during tectonic burial in the Western Alps.
Luke N. J. Wedmore, Tess Turner, Juliet Biggs, Jack N. Williams, Henry M. Sichingabula, Christine Kabumbu, and Kawawa Banda
Solid Earth, 13, 1731–1753, https://doi.org/10.5194/se-13-1731-2022, https://doi.org/10.5194/se-13-1731-2022, 2022
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Mapping and compiling the attributes of faults capable of hosting earthquakes are important for the next generation of seismic hazard assessment. We document 18 active faults in the Luangwa Rift, Zambia, in an active fault database. These faults are between 9 and 207 km long offset Quaternary sediments, have scarps up to ~30 m high, and are capable of hosting earthquakes from Mw 5.8 to 8.1. We associate the Molaza Fault with surface ruptures from two unattributed M 6+ 20th century earthquakes.
Michał P. Michalak, Lesław Teper, Florian Wellmann, Jerzy Żaba, Krzysztof Gaidzik, Marcin Kostur, Yuriy P. Maystrenko, and Paulina Leonowicz
Solid Earth, 13, 1697–1720, https://doi.org/10.5194/se-13-1697-2022, https://doi.org/10.5194/se-13-1697-2022, 2022
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When characterizing geological/geophysical surfaces, various geometric attributes are calculated, such as dip angle (1D) or dip direction (2D). However, the boundaries between specific values may be subjective and without optimization significance, resulting from using default color palletes. This study proposes minimizing cosine distance among within-cluster observations to detect 3D anomalies. Our results suggest that the method holds promise for identification of megacylinders or megacones.
Erik M. Young, Christie D. Rowe, and James D. Kirkpatrick
Solid Earth, 13, 1607–1629, https://doi.org/10.5194/se-13-1607-2022, https://doi.org/10.5194/se-13-1607-2022, 2022
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Studying how earthquakes spread deep within the faults they originate from is crucial to improving our understanding of the earthquake process. We mapped preserved ancient earthquake surfaces that are now exposed in South Africa and studied their relationship with the shape and type of rocks surrounding them. We determined that these surfaces are not random and are instead associated with specific kinds of rocks and that their shape is linked to the evolution of the faults in which they occur.
Sivaji Lahiri, Kitty L. Milliken, Peter Vrolijk, Guillaume Desbois, and Janos L. Urai
Solid Earth, 13, 1513–1539, https://doi.org/10.5194/se-13-1513-2022, https://doi.org/10.5194/se-13-1513-2022, 2022
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Understanding the mechanism of mechanical compaction is important. Previous studies on mechanical compaction were mostly done by performing experiments. Studies on natural rocks are rare due to compositional heterogeneity of the sedimentary succession with depth. Due to remarkable similarity in composition and grain size, the Sumatra subduction complex provides a unique opportunity to study the micromechanism of mechanical compaction on natural samples.
Dongwon Lee, Nikolaos Karadimitriou, Matthias Ruf, and Holger Steeb
Solid Earth, 13, 1475–1494, https://doi.org/10.5194/se-13-1475-2022, https://doi.org/10.5194/se-13-1475-2022, 2022
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This research article focuses on filtering and segmentation methods employed in high-resolution µXRCT studies for crystalline rocks, bearing fractures, or fracture networks, of very small aperture. Specifically, we focus on the identification of artificially induced (via quenching) fractures in Carrara marble samples. Results from the same dataset from all five different methods adopted were produced and compared with each other in terms of their output quality and time efficiency.
Alberto Ceccato, Giulia Tartaglia, Marco Antonellini, and Giulio Viola
Solid Earth, 13, 1431–1453, https://doi.org/10.5194/se-13-1431-2022, https://doi.org/10.5194/se-13-1431-2022, 2022
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The Earth's surface is commonly characterized by the occurrence of fractures, which can be mapped, and their can be geometry quantified on digital representations of the surface at different scales of observation. Here we present a series of analytical and statistical tools, which can aid the quantification of fracture spatial distribution at different scales. In doing so, we can improve our understanding of how fracture geometry and geology affect fluid flow within the fractured Earth crust.
Giulio Viola, Giovanni Musumeci, Francesco Mazzarini, Lorenzo Tavazzani, Manuel Curzi, Espen Torgersen, Roelant van der Lelij, and Luca Aldega
Solid Earth, 13, 1327–1351, https://doi.org/10.5194/se-13-1327-2022, https://doi.org/10.5194/se-13-1327-2022, 2022
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A structural-geochronological approach helps to unravel the Zuccale Fault's architecture. By mapping its internal structure and dating some of its fault rocks, we constrained a deformation history lasting 20 Myr starting at ca. 22 Ma. Such long activity is recorded by now tightly juxtaposed brittle structural facies, i.e. different types of fault rocks. Our results also have implications on the regional evolution of the northern Apennines, of which the Zuccale Fault is an important structure.
Wan-Lin Hu
Solid Earth, 13, 1281–1290, https://doi.org/10.5194/se-13-1281-2022, https://doi.org/10.5194/se-13-1281-2022, 2022
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Having a seismic image is generally expected to enable us to better determine fault geometry and thus estimate geological slip rates accurately. However, the process of interpreting seismic images may introduce unintended uncertainties, which have not yet been widely discussed. Here, a case of a shear fault-bend fold in the frontal Himalaya is used to demonstrate how differences in interpretations can affect the following estimates of slip rates and dependent conclusions.
Manuel D. Menzel, Janos L. Urai, Estibalitz Ukar, Thierry Decrausaz, and Marguerite Godard
Solid Earth, 13, 1191–1218, https://doi.org/10.5194/se-13-1191-2022, https://doi.org/10.5194/se-13-1191-2022, 2022
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Mantle rocks can bind large quantities of carbon by reaction with CO2, but this capacity requires fluid pathways not to be clogged by carbonate. We studied mantle rocks from Oman to understand the mechanisms allowing their transformation into carbonate and quartz. Using advanced imaging techniques, we show that abundant veins were essential fluid pathways driving the reaction. Our results show that tectonic stress was important for fracture opening and a key ingredient for carbon fixation.
Jean-Baptiste P. Koehl, Steffen G. Bergh, and Arthur G. Sylvester
Solid Earth, 13, 1169–1190, https://doi.org/10.5194/se-13-1169-2022, https://doi.org/10.5194/se-13-1169-2022, 2022
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The San Andreas fault is a major active fault associated with ongoing earthquake sequences in southern California. The present study investigates the development of the Indio Hills area in the Coachella Valley along the main San Andreas fault and the Indio Hills fault. The Indio Hills area is located near an area with high ongoing earthquake activity (Brawley seismic zone), and, therefore, its recent tectonic evolution has implications for earthquake prediction.
Jin Lai, Dong Li, Yong Ai, Hongkun Liu, Deyang Cai, Kangjun Chen, Yuqiang Xie, and Guiwen Wang
Solid Earth, 13, 975–1002, https://doi.org/10.5194/se-13-975-2022, https://doi.org/10.5194/se-13-975-2022, 2022
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(1) Structural diagenesis analysis is performed on the ultra-deep tight sandstone. (2) Fracture and intergranular pores are related to the low in situ stress magnitudes. (3) Dissolution is associated with the presence of fracture.
Hamed Fazlikhani, Wolfgang Bauer, and Harald Stollhofen
Solid Earth, 13, 393–416, https://doi.org/10.5194/se-13-393-2022, https://doi.org/10.5194/se-13-393-2022, 2022
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Interpretation of newly acquired FRANKEN 2D seismic survey data in southeeastern Germany shows that upper Paleozoic low-grade metasedimentary rocks and possible nappe units are transported by Variscan shear zones to ca. 65 km west of the Franconian Fault System (FFS). We show that the locations of post-Variscan upper Carboniferous–Permian normal faults and associated graben and half-graben basins are controlled by the geometry of underlying Variscan shear zones.
Xiaodong Ma, Marian Hertrich, Florian Amann, Kai Bröker, Nima Gholizadeh Doonechaly, Valentin Gischig, Rebecca Hochreutener, Philipp Kästli, Hannes Krietsch, Michèle Marti, Barbara Nägeli, Morteza Nejati, Anne Obermann, Katrin Plenkers, Antonio P. Rinaldi, Alexis Shakas, Linus Villiger, Quinn Wenning, Alba Zappone, Falko Bethmann, Raymi Castilla, Francisco Seberto, Peter Meier, Thomas Driesner, Simon Loew, Hansruedi Maurer, Martin O. Saar, Stefan Wiemer, and Domenico Giardini
Solid Earth, 13, 301–322, https://doi.org/10.5194/se-13-301-2022, https://doi.org/10.5194/se-13-301-2022, 2022
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Questions on issues such as anthropogenic earthquakes and deep geothermal energy developments require a better understanding of the fractured rock. Experiments conducted at reduced scales but with higher-resolution observations can shed some light. To this end, the BedrettoLab was recently established in an existing tunnel in Ticino, Switzerland, with preliminary efforts to characterize realistic rock mass behavior at the hectometer scale.
Berit Schwichtenberg, Florian Fusseis, Ian B. Butler, and Edward Andò
Solid Earth, 13, 41–64, https://doi.org/10.5194/se-13-41-2022, https://doi.org/10.5194/se-13-41-2022, 2022
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Hydraulic rock properties such as porosity and permeability are relevant factors that have an impact on groundwater resources, geological repositories and fossil fuel reservoirs. We investigate the influence of chemical compaction upon the porosity evolution in salt–biotite mixtures and related transport length scales by conducting laboratory experiments in combination with 4-D analysis. Our observations invite a renewed discussion of the effect of sheet silicates on chemical compaction.
David Healy and Stephen Paul Hicks
Solid Earth, 13, 15–39, https://doi.org/10.5194/se-13-15-2022, https://doi.org/10.5194/se-13-15-2022, 2022
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The energy transition requires operations in faulted rocks. To manage the technical challenges and public concern over possible induced earthquakes, we need to quantify the risks. We calculate the probability of fault slip based on uncertain inputs, stresses, fluid pressures, and the mechanical properties of rocks in fault zones. Our examples highlight the specific gaps in our knowledge. Citizen science projects could produce useful data and include the public in the discussions about hazards.
Manuel I. de Paz-Álvarez, Thomas G. Blenkinsop, David M. Buchs, George E. Gibbons, and Lesley Cherns
Solid Earth, 13, 1–14, https://doi.org/10.5194/se-13-1-2022, https://doi.org/10.5194/se-13-1-2022, 2022
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We describe a virtual geological mapping course implemented in response to travelling and social restrictions derived from the ongoing COVID-19 pandemic. The course was designed to replicate a physical mapping exercise as closely as possible with the aid of real field data and photographs collected by the authors during previous years in the Cantabrian Zone (NW Spain). The course is delivered through Google Earth via a KMZ file with outcrop descriptions and links to GitHub-hosted photographs.
Yueyang Xia, Jacob Geersen, Dirk Klaeschen, Bo Ma, Dietrich Lange, Michael Riedel, Michael Schnabel, and Heidrun Kopp
Solid Earth, 12, 2467–2477, https://doi.org/10.5194/se-12-2467-2021, https://doi.org/10.5194/se-12-2467-2021, 2021
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The 2 June 1994 Java tsunami earthquake ruptured in a seismically quiet subduction zone and generated a larger-than-expected tsunami. Here, we re-process a seismic line across the rupture area. We show that a subducting seamount is located up-dip of the mainshock in a region that did not rupture during the earthquake. Seamount subduction modulates the topography of the marine forearc and acts as a seismic barrier in the 1994 earthquake rupture.
Steffen Abe and Hagen Deckert
Solid Earth, 12, 2407–2424, https://doi.org/10.5194/se-12-2407-2021, https://doi.org/10.5194/se-12-2407-2021, 2021
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We use numerical simulations and laboratory experiments on rock samples to investigate how stress conditions influence the geometry and roughness of fracture surfaces. The roughness of the surfaces was analyzed in terms of absolute roughness and scaling properties. The results show that the surfaces are self-affine but with different scaling properties between the numerical models and the real rock samples. Results suggest that stress conditions have little influence on the surface roughness.
Cited articles
Abercrombie, R. E. and Ekström, G.: Earthquake slip on oceanic transform faults, Nature, 410, 74–77, 2001.
Abercrombie, R. E. and Ekström, G.: A reassessment of the rupture characteristics of oceanic transform earthquakes, J. Geophys. Res., 108, 2225, 2003.
Atkinson, H. V.: Overview no. 65: Theories of normal grain growth in pure single phase systems, Acta Metall., 36, 469–491, 1988.
Avrami, M.: Kinetics of phase change. I General theory, The Journal of Chemical Physics, 7, 1103–1112, 1939.
Avrami, M.: Kinetics of phase change. II Transformation-time relations for random distribution of nuclei, The Journal of Chemical Physics, 8, 212–224, 1940.
Avrami, M.: Granulation, phase change, and microstructure kinetics of phase change. III, The Journal of Chemical Physics, 9, 177–184, 1941.
Baluffi, R. W., Komen, Y., and Schober, T.: Electron microscope studies of grain boundary dislocation behaviour, Surf. Sci, 31, 68–103, 1972.
Ben-Zion, Y., and Lyakhovsky, V.: Analysis of aftershocks in a lithospheric model with seismogenic zone governed by damage rheology, Geophys. J. Int., 165, 197–210, 2006.
Ben-Zion, Y.: Collective behavior of earthquakes and faults: continuum-discrete transitions, progressive evolutionary changes, and different dynamic regimes, Rev. Geophys., 46, RG4006, https://doi.org/10.1029/2008RG000260, 2008.
Birtel, S. and Stöckhert, B.: Quartz veins record earthquake-related brittle failure and short term ductile flow in the deep crust, Tectonophysics, 457, 53–63, 2008.
Boettcher, M. S., Hirth, G., and Evans, B.: Olivine friction at the base of oceanic seismogenic zones, J. Geophys. Res., 112, B01205, https://doi.org/10.1029/2006JB004301, 2007.
Chopra, P. N. and Paterson, M. S.: The experimental deformation of dunite, Tectonophysics, 78, 453–473, 1981.
Christian, J. W.: The Theory of Transformations in Metals and Alloys: Part I + II, Elsevier Science Ltd, Oxford, 2002.
Cooper, R. F. and Kohlstedt, D. L.: Interfacial energies in the olivine-basalt system, Adv. Earth Planet. Sci, 12, 217–228, 1982.
Deer, W. A., Howie, R. A., and Zussman, J.: An introduction to the Rock-forming Minerals, Longman, Essex, 1, 528, 1992.
Dessa, J. X., Klingelhoefer, F., Graindorge, D., André, C., Permana, H., Gutscher, M. A., Chauhan, A., and Singh, S. C.: Megathrust earthquakes can nucleate in the forearc mantle: evidence from the 2004 Sumatra event, Geology, 37, https://doi.org/10.1130/G25653A, 2009.
Dohmen, R., Chakraborty, S., and Becker, H. W.: Si and O diffusion in olivine and implications for characterizing plastic flow in the mantle, Geophys. Res. Lett., 29, 2030, https://doi.org/10.1029/2002GL015480, 2002.
Drolet, J. and Galibois, A.: Altering the time cycle of heat treatment by preannealing prior to grain growth, Metall. Mater. Trans. B, 2, 53–64, 1971.
Druiventak, A., Trepmann, C. A., Renner, J., and Hanke, K.: Low-temperature plasticity of olivine during high stress deformation of peridotite at lithospheric conditions – An experimental study, Earth Planet. Sci. Lett., 311, 199–211, 2011.
Druiventak, A., Matysiak, A., Renner, J., and Trepmann, C. A.: Kick-and-cook experiments on peridotite: simulating coseismic deformation and post-seismic creep, Terra Nova, 24, 62–69, 2012.
Drury, M. R. and Urai, J. L.: Deformation-related recrystallization processes, Tectonophysics, 172, 235–253, 1990.
Durinck, J., Devincre, B., Kubin, L., and Cordier, P.: Modeling the plastic deformation of olivine by dislocation dynamics simulations, Am. Min., 92, 1346–1357, 2007.
Duyster, J. and Stöckhert, B.: Grain boundary energies in olivine derived from natural microstructures, Contributions to Mineralogy and Petrology, 140, 567–576, 2001.
Ellis, S. and Stöckhert, B.: Elevated stresses and creep rates beneath the brittle-ductile transition caused by seismic faulting in the upper crust, J. Geophys. Res, 109, B05407, https://doi.org/10.1029/2003JB002744, 2004.
Evans, B. E., Renner, J. R., and Hirth, G. H.: A few remarks on the kinetics of static grain growth in rocks, Int. J. Earth Sci., 90, 88–103, 2001.
Farla, R., Kokkonen, H., Fitz Gerald, J., Barnhoorn, A., Faul, U., and Jackson, I.: Dislocation recovery in fine-grained polycrystalline olivine, Physics and Chemistry of Minerals, 38, 363–377, 2011.
Fitz Gerald, J. D. and Stünitz, H.: Deformation of granitoids at low metamorphic grade. I: Reactions and grain size reduction, Tectonophysics, 221, 269–297, 1993.
Fredrich, J. T., Evans, B., and Wong, T.-F.: Effect of grain size on brittle and semibrittle strength: Implications for micromechanical modelling of failure in compression, J. Geophys. Res., 95, 10907–10920, https://doi.org/10.1029/JB095iB07p10907, 1990.
Hackl, K. and Renner, J.: High-temperature deformation and recrystallization: a variational analysis and its application to olivine aggregates, J. Geophys. Res., 118, 943–967, https://doi.org/10.1002/jgrb.50125, 2013.
Hall, E. O.: The Deformation and Ageing of Mild Steel: III Discussion of Results, Proc. Phys. Soc. B., 64, 747–753, 1951.
Hirth, J.: The influence of grain boundaries on mechanical properties, Metall. Mater. Trans. B, 3, 3047–3067, 1972.
Hirth, G. and Kohlstedt, D.: Rheology of the upper mantle and the mantle wedge: a view from the experimentalists, in: Inside the Subduction Factory, edited by: Eiler, J., Geophys. Monogr., AGU, Washington, 83–105, 2003.
Hobbs, B. E.: Recrystallisation of single crystals of quartz, Tectonophysics 6, 353–401, 1968.
Holyoke III, C. W., and Kronenberg, A. K.: Accurate differential stress measurement using the molten salt cell and solid salt assemblies in the Griggs apparatus with applications to strength, piezometers and rheology, Tectonophysics, 494, 17–31, 2010.
Humphreys, F. J., and Hatherly, M.: Recrystallization and related annealing phenomena, 2 Edn., Elsevier Ltd, Oxford, 605 pp., 2004.
Jackson, I., Fitz Gerald, J. D., Faul, U. H., and Tan, B. H.: Grain-size-sensitive seismic wave attenuation in polycrystalline olivine, J. Geophys. Res.-Sol. Ea., 107, 2360, https://doi.org/10.1029/2001JB001225, 2002.
Jaroslow, G. E., Hirth, G., and Dick, H. J. B.: Abyssal peridotite mylonites: implications for grain-size sensitive flow and strain localization in the oceanic lithosphere, Tectonophysics, 256, 17–37, 1996.
Johnson, W. A. and Mehl, R. F.: Reaction kinetics in processes of nucleation and growth, Trans. Am. Inst. Min. Metall. Engrs, 135, 416–458, 1939.
Kaminski, É. and Ribe, N. M.: A kinematic model for recrystallization and texture development in olivine polycrystals, Earth Planet. Sci. Lett., 189, 253–267, 2001.
Karato, S. and Ogawa, M.: High-pressure recovery of olivine: implications for creep mechanisms and creep activation volume, Phys. Earth Planet. Int., 28, 102–117, 1982.
Karato, S., Rubie, D. C., and Yan, H.: Dislocation Recovery in Olivine Under Deep Upper Mantle Conditions: Implications for Creep and Diffusion, J. Geophys. Res., 98, 9761–9768, 1993.
Karato, S.: Grain growth kinetics in olivine aggregates, Tectonophysics, 168, 255–273, 1989.
Kempen, A. T. W., Sommer, F., and Mittemeijer, E. J.: The isothermal and isochronal kinetics of the crystallisation of bulk amorphous Pd40Cu30P20Ni10, Acta materialia, 50, 1319–1329, 2002.
Kohlstedt, D. L., Nichols, H. P. K., and Hornack, P.: The Effect of Pressure on the Rate of Dislocation Recovery in Olivine, J. Geophys. Res., 85, 3122–3130, 1980.
Küster, M., and Stöckhert, B.: High differential stress and sublithostatic pore fluid pressure in the ductile regime – microstructural evidence for short-term post-seismic creep in the Sesia Zone, Western Alps, Tectonophysics, 303, 263–277, 1999.
Liu, M. and Evans, B.: Dislocation recovery kinetics in single-crystal calcite, J. Geophys. Res., 102, 24801–24809, 1997.
Liu, F., Sommer, F., and Mittemeijer, E. J.: An analytical model for isothermal and isochronal transformation kinetics, J. Mat. Sci., 39, 1621–1634, 2004.
Luo, H.: Effect of concurrent recovery on Avrami exponent of the softening kinetics after hot deformation, Mat. Sci. Engineer. A, 532, 44–49, 2012.
Matysiak, A. K. and Trepmann, C. A.: Crystal-plastic deformation and recrystallization of peridotite controlled by the seismic cycle, Tectonophysics, 530–531, 111–127, 2012.
McKenzie, D., Jackson, J., and Priestley, K.: Thermal structure of oceanic and continental lithosphere, Earth Planet. Sci. Lett., 233, 337–349, 2005.
Moghadam, R. H., Trepmann, C. A., Stöckhert, B., and Renner, J.: Rheology of synthetic omphacite aggregates at high pressure and high temperature, J. Petrology, 51, 92-1-945, 2010.
Nes, E.: Recovery revisited, Acta Metallurgica et Materialia, 43, 2189–2207, 1995.
Nicolas, A. and Poirier, J. P.: Crystalline Plasticity and Solid State Flow in Metamorphic Rocks, John Wiley, New York, 444 pp., 1976.
Nüchter, J.-A. and Stöckhert, B.: Vein quartz microfabrics indicating progressive evolution of fractures into cavities during postseismic creep in the middle crust, J. Struct. Geol., 29, 1445–1462, 2007.
Nüchter, J.-A. and Ellis, S.: Complex states of stress during the normal faulting seismic cycle: role of midcrustal postseismic creep, J. Geophys. Res., 115, B12411, https://doi.org/10.1029/2010JB007557, 2010.
Orzol, J., Stöckhert, B., Trepmann, C. A., and Rummel, F.: Experimental deformation of synthetic wet jadeite aggregates, J. Geophys. Res., 111, B06205, 2006.
Passchier, C. W. and Trouw, R. A. J.: Microtectonics, 2nd ed., Springer Verlag, Berlin-Heidelberg-New York, 2008.
Petch, N. J.: The cleavage strength of polycrystals, Journal of the Iron Steel Institute London, 174, 25–28, 1953.
Piazolo, S., Bestmann, M., Prior, D. J., and Spiers, C. J.: Temperature dependent grain boundary migration in deformed-then-annealed material: Observations from experimentally deformed synthetic rocksalt, Tectonophysics 427, 55–71, 2006.
Platt, J. P. and Behr, W. M.: Grainsize evolution in ductile shear zones: Implications for strain localization and the strength of the lithosphere, J. Struct. Geol., 33, 537–550, 2011a.
Platt, J. P. and Behr, W. M.: Lithospheric shear zones as constant stress experiments, Geology, 39, 127–130, 2011b.
Renner, J., Zerbian, A., and Stöckhert, B.: Microstructures of synthetic polycrystalline coesite aggregates, The effect of pressure, temperature, and time, Lithos, 41, 169–184, 1997.
Rolandone, F., Bürgmann, R., and Nadeau, R. M.: The evolution of the seismic-aseismic transition during the earthquake cycle: constraints from the time-dependent depth distribution of aftershocks, Geophys. Res. Lett., 31, L23610, https://doi.org/10.1029/2004GL021379, 2004.
Rybacki, E., Renner, J., Konrad, K., Harbott, W., Rummel, F., and Stöckhert, B.: A Servohydraulically-controlled Deformation Apparatus for Rock Deformation under Conditions of Ultra-high Pressure Metamorphism, Pure Appl. Geophys., 152, 579–606, 1998.
Schaff, D. P., Bokelmann, G. H. R., Beroza, G. C., Waldhauser, F., and Ellsworth, W. L.: High-resolution image of Calaveras Fault seismicity, J. Geophys. Res.-Sol. Ea., 107, 2186, https://doi.org/10.1029/2001JB000633, 2002.
Scholz, C. H.: The mechanics of earthquakes and faulting. Cambridge University press, Cambridge, 2 Edn., 2002.
Shimizu, I.: Stress and temperature dependence of recrystallized grain size: a subgrain misorientation model, Geophys. Res. Lett., 25, 4237–4240, 1998.
Sibson, R. H.: Transient discontinuities in ductile shear zones, J. Struct. Geol., 2, 165–171, 1980.
Simpson, C. J. and Aust, K. T.: Grain boundary migration, Surface Science, 31, 479–497, 1972.
Singh, S. C., Carton, H., Tapponnier, P., Hananto, N. D., Chauhan, A. P. S., Hartoyo, D., Bayly, M., Moeljopranoto, S., Bunting, T., and Christie, P.: Seismic evidence for broken oceanic crust in the 2004 Sumatra earthquake epicentral region, Nat. Geosci., 1, 777–781, 2008.
Stipp, M. and Kunze, K.: Dynamic recrystallization near the brittle-plastic transition in naturally and experimentally deformed quartz aggregates, Tectonophysics, 448, 77–97, 2008.
Stünitz, H., Fitz Gerald, J. D., and Tullis, J.: Dislocation generation, slip systems, and dynamic recrystallization in experimentally deformed plagioclase single crystals, Tectonophysics, 372, 215–233, 2003.
Toriumi, M. and Karato, S.: Experimental studies on the recovery process of deformed olivines and the mechanical state of the upper mantle, Tectonophysics, 49, 79–95, 1978.
Toriumi, M.: Grain boundary migration in olivine at atmospheric pressure, Phys. Earth Planet. Int., 30, 26–35, 1982.
Trepmann, C. A. and Stöckhert, B.: Mechanical twinning of jadeite – an indication of synseismic loading beneath the brittle-plastic transition, Int. J. Earth Sci., 90, 4–13, 2001.
Trepmann, C. A. and Stöckhert, B.: Cataclastic deformation of garnet: a record of synseismic loading and postseismic creep, J. Struct. Geol., 24, 1845–1856, 2002.
Trepmann, C. A. and Stöckhert, B.: Quartz microstructures developed during non-steady state plastic flow at rapidly decaying stress and strain rate, J. Struct. Geol., 25, 2035–2051, 2003.
Trepmann, C. A., Stöckhert, B., Dorner, D., Moghadam, R. H., Küster, M., and Röller, K.: Simulating coseismic deformation of quartz in the middle crust and fabric evolution during postseismic stress relaxation – An experimental study, Tectonophysics, 442, 83–104, 2007.
Trepmann, C. A. and Stöckhert, B.: Short-wavelength undulatory extinction in quartz recording coseismic deformation in the middle crust – an experimental study, Solid Earth, 4, 263–276, https://doi.org/10.5194/se-4-263-2013, 2013.
Urai, J. L. and Humphreys, F. J.: A collection of time-lapse movies from transmitted light deformation experiments, in: Stress, Strain and Structure, A volume in honour of W. D. Means, edited by: Jessell, M. W. and Urai, J. L., Vol. 2, J. Virtual Explor., 2000.
Vandermeer, R. A., Jensen, D. J., and Woldt, E.: Grain boundary mobility during recrystallization of copper, Metall. Mater. Trans. A, 28, 749–754, 1997.
Warren, J. M. and Hirth, G.: Grain size sensitive deformation mechanisms in naturally deformed peridotites, Earth Planet. Sci. Lett., 248, 438–450, 2006.
