Articles | Volume 11, issue 6
https://doi.org/10.5194/se-11-2141-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-11-2141-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Relationship between microstructures and resistance in mafic assemblages that deform and transform
Institut des Sciences de la Terre d'Orléans (ISTO), UMR 7327,
CNRS/BRGM, Université d'Orléans, 45071 Orléans, France
Holger Stünitz
Institut des Sciences de la Terre d'Orléans (ISTO), UMR 7327,
CNRS/BRGM, Université d'Orléans, 45071 Orléans, France
Department of Geology, University of Tromsø, Dramsveien 201, 9037
Tromsø, Norway
Hugues Raimbourg
Institut des Sciences de la Terre d'Orléans (ISTO), UMR 7327,
CNRS/BRGM, Université d'Orléans, 45071 Orléans, France
Jacques Précigout
Institut des Sciences de la Terre d'Orléans (ISTO), UMR 7327,
CNRS/BRGM, Université d'Orléans, 45071 Orléans, France
Alexis Plunder
BRGM, 45060 Orléans, France
Lucille Nègre
Institut des Sciences de la Terre d'Orléans (ISTO), UMR 7327,
CNRS/BRGM, Université d'Orléans, 45071 Orléans, France
Related authors
No articles found.
Vincent Famin, Hugues Raimbourg, Muriel Andreani, and Anne-Marie Boullier
Solid Earth, 12, 2067–2085, https://doi.org/10.5194/se-12-2067-2021, https://doi.org/10.5194/se-12-2067-2021, 2021
Short summary
Short summary
Sediments accumulated in accretionary prisms are deformed by the compression imposed by plate subduction. Here we show that deformation of the sediments transforms some minerals in them. We suggest that these mineral transformations are due to the proliferation of microorganisms boosted by deformation. Deformation-enhanced microbial proliferation may change our view of sedimentary and tectonic processes in subduction zones.
Junichi Fukuda, Hugues Raimbourg, Ichiko Shimizu, Kai Neufeld, and Holger Stünitz
Solid Earth, 10, 621–636, https://doi.org/10.5194/se-10-621-2019, https://doi.org/10.5194/se-10-621-2019, 2019
Short summary
Short summary
Grain size is a key factor for deformation. Quartz is one of the main constituents of the crust, but little is known about grain growth that can change grain size. We therefore experimentally determined grain growth laws for quartz. We discuss the importance of the grain size exponent, water fugacity exponent, and activation energy. Our results indicate that the contribution of grain growth to deformation may become important in lower-crustal conditions.
Carly Faber, Holger Stünitz, Deta Gasser, Petr Jeřábek, Katrin Kraus, Fernando Corfu, Erling K. Ravna, and Jiří Konopásek
Solid Earth, 10, 117–148, https://doi.org/10.5194/se-10-117-2019, https://doi.org/10.5194/se-10-117-2019, 2019
Short summary
Short summary
The Caledonian mountains formed when Baltica and Laurentia collided around 450–400 million years ago. This work describes the history of the rocks and the dynamics of that continental collision through space and time using field mapping, estimated pressures and temperatures, and age dating on rocks from northern Norway. The rocks preserve continental collision between 440–430 million years ago, and an unusual pressure–temperature evolution suggests unusual tectonic activity prior to collision.
Sina Marti, Holger Stünitz, Renée Heilbronner, Oliver Plümper, and Rüdiger Kilian
Solid Earth, 9, 985–1009, https://doi.org/10.5194/se-9-985-2018, https://doi.org/10.5194/se-9-985-2018, 2018
Short summary
Short summary
Using rock deformation experiments we study how rocks deform at mid-crustal levels within mountain belts and along plate boundaries. For the studied material, fluid-assisted mass transport and grain sliding are the dominant deformation mechanisms when small amounts of water are present. Our results provide new data on the mechanical response of the earth's crust, and the wide range of presented microstructures will help to correlate observations from experiments and nature.
Alexis Plunder, Cédric Thieulot, and Douwe J. J. van Hinsbergen
Solid Earth, 9, 759–776, https://doi.org/10.5194/se-9-759-2018, https://doi.org/10.5194/se-9-759-2018, 2018
Short summary
Short summary
The thermal state of the Earth's crust determines how it reacts to tectonic forces and to fluid flow responsible for ore formation. We hypothesize that the angle between plate motion and convergent boundaries determines the thermal regime of subduction zones (where a plate goes under another one). Computer models and a geological reconstruction of Turkey were used to validate this hypothesis.
This research was done to validate a hypothesis made on the basis of nonquantitative field data.
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: Structural geology
Driven magmatism and crustal thinning of coastal southern China in response to subduction
Selection and characterization of the target fault for fluid-induced activation and earthquake rupture experiments
Naturally fractured reservoir characterisation in heterogeneous sandstones: insight for uranium in situ recovery (Imouraren, Niger)
Influence of water on crystallographic preferred orientation patterns in a naturally-deformed quartzite
Multiscalar 3D temporal structural characterisation of Smøla island, mid-Norwegian passive margin: an analogue for unravelling the tectonic history of offshore basement highs
Localized shear versus distributed strain accumulation as shear-accommodation mechanisms in ductile shear zones: Constraining their dictating factors
Impact of faults on the remote stress state
Subduction plate interface shear stress associated with rapid subduction at deep slow earthquake depths: example from the Sanbagawa belt, southwestern Japan
Multiple phase rifting and subsequent inversion in the West Netherlands Basin: implications for geothermal reservoir characterization
Analogue modelling of basin inversion: implications for the Araripe Basin (Brazil)
Geomorphic expressions of active rifting reflect the role of structural inheritance: A new model for the evolution of the Shanxi Rift, North China
Natural fracture patterns at Swift Reservoir anticline, NW Montana: the influence of structural position and lithology from multiple observation scales
Rapid hydration and weakening of anhydrite under stress: implications for natural hydration in the Earth's crust and mantle
Analogue experiments on releasing and restraining bends and their application to the study of the Barents Shear Margin
Structural framework and timing of the Pahtohavare Cu ± Au deposits, Kiruna mining district, Sweden
Does the syn- versus post-rift thickness ratio have an impact on the inversion-related structural style?
Inversion of accommodation zones in salt-bearing extensional systems: insights from analog modeling
Structural control of inherited salt structures during inversion of a domino basement-fault system from an analogue modelling approach
Kinematics and time-resolved evolution of the main thrust-sense shear zone in the Eo-Alpine orogenic wedge (the Vinschgau Shear Zone, eastern Alps)
Role of inheritance during tectonic inversion of a rift system in basement-involved to salt-decoupled transition: analogue modelling and application to the Pyrenean–Biscay system
Water release and homogenization by dynamic recrystallization of quartz
Hydrothermal activity of the Lake Abhe geothermal field (Djibouti): Structural controls and paths for further exploration
Time-dependent frictional properties of granular materials used in analogue modelling: implications for mimicking fault healing during reactivation and inversion
Large grain-size-dependent rheology contrasts of halite at low differential stress: evidence from microstructural study of naturally deformed gneissic Zechstein 2 rock salt (Kristallbrockensalz) from the northern Netherlands
Analogue modelling of the inversion of multiple extensional basins in foreland fold-and-thrust belts
A contribution to the quantification of crustal shortening and kinematics of deformation across the Western Andes ( ∼ 20–22° S)
Rift thermal inheritance in the SW Alps (France): insights from RSCM thermometry and 1D thermal numerical modelling
The Luangwa Rift Active Fault Database and fault reactivation along the southwestern branch of the East African Rift
Clustering has a meaning: optimization of angular similarity to detect 3D geometric anomalies in geological terrains
Shear zone evolution and the path of earthquake rupture
Mechanical compaction mechanisms in the input sediments of the Sumatra subduction complex – insights from microstructural analysis of cores from IODP Expedition 362
Detecting micro fractures: a comprehensive comparison of conventional and machine-learning-based segmentation methods
Multiscale lineament analysis and permeability heterogeneity of fractured crystalline basement blocks
Structural characterization and K–Ar illite dating of reactivated, complex and heterogeneous fault zones: lessons from the Zuccale Fault, Northern Apennines
How do differences in interpreting seismic images affect estimates of geological slip rates?
Progressive veining during peridotite carbonation: insights from listvenites in Hole BT1B, Samail ophiolite (Oman)
Tectonic evolution of the Indio Hills segment of the San Andreas fault in southern California, southwestern USA
Structural diagenesis in ultra-deep tight sandstones in the Kuqa Depression, Tarim Basin, China
Variscan structures and their control on latest to post-Variscan basin architecture: insights from the westernmost Bohemian Massif and southeastern Germany
Multi-disciplinary characterizations of the BedrettoLab – a new underground geoscience research facility
Biotite supports long-range diffusive transport in dissolution–precipitation creep in halite through small porosity fluctuations
De-risking the energy transition by quantifying the uncertainties in fault stability
Virtual field trip to the Esla Nappe (Cantabrian Zone, NW Spain): delivering traditional geological mapping skills remotely using real data
Marine forearc structure of eastern Java and its role in the 1994 Java tsunami earthquake
Roughness of fracture surfaces in numerical models and laboratory experiments
Impact of basement thrust faults on low-angle normal faults and rift basin evolution: a case study in the Enping sag, Pearl River Basin
Evidence for and significance of the Late Cretaceous Asteroussia event in the Gondwanan Ios basement terranes
Investigating spatial heterogeneity within fracture networks using hierarchical clustering and graph distance metrics
Dating folding beyond folding, from layer-parallel shortening to fold tightening, using mesostructures: lessons from the Apennines, Pyrenees, and Rocky Mountains
Deformation-enhanced diagenesis and bacterial proliferation in the Nankai accretionary prism
Jinbao Su, Wenbin Zhu, and Guangwei Li
Solid Earth, 15, 1133–1141, https://doi.org/10.5194/se-15-1133-2024, https://doi.org/10.5194/se-15-1133-2024, 2024
Short summary
Short summary
The late Mesozoic igneous rocks in the South China Block exhibit flare-ups and lulls, which form in compressional or extensional backgrounds. The ascending of magma forms a mush-like head and decreases crustal thickness. The presence of faults and pre-existing magmas will accelerate emplacement of underplating magma. The magmatism at different times may be formed under similar subduction conditions, and the boundary compression forces will delay magma ascent.
Peter Achtziger-Zupančič, Alberto Ceccato, Alba Simona Zappone, Giacomo Pozzi, Alexis Shakas, Florian Amann, Whitney Maria Behr, Daniel Escallon Botero, Domenico Giardini, Marian Hertrich, Mohammadreza Jalali, Xiaodong Ma, Men-Andrin Meier, Julian Osten, Stefan Wiemer, and Massimo Cocco
Solid Earth, 15, 1087–1112, https://doi.org/10.5194/se-15-1087-2024, https://doi.org/10.5194/se-15-1087-2024, 2024
Short summary
Short summary
We detail the selection and characterization of a fault zone for earthquake experiments in the Fault Activation and Earthquake Ruptures (FEAR) project at the Bedretto Lab. FEAR, which studies earthquake processes, overcame data collection challenges near faults. The fault zone in Rotondo granite was selected based on geometry, monitorability, and hydro-mechanical properties. Remote sensing, borehole logging, and geological mapping were used to create a 3D model for precise monitoring.
Maxime Jamet, Gregory Ballas, Roger Soliva, Olivier Gerbeaud, Thierry Lefebvre, Christine Leredde, and Didier Loggia
Solid Earth, 15, 895–920, https://doi.org/10.5194/se-15-895-2024, https://doi.org/10.5194/se-15-895-2024, 2024
Short summary
Short summary
This study characterizes the Tchirezrine II sandstone reservoir in northern Niger. Crucial for potential uranium in situ recovery (ISR), our multifaceted approach reveals (i) a network of homogeneously distributed orthogonal structures, (ii) the impact of clustered E–W fault structures on anisotropic fluid flow, and (iii) local changes in the matrix behaviour of the reservoir as a function of the density and nature of the deformation structure.
Jeffrey M. Rahl, Brendan Moehringer, Kenneth S. Befus, and John S. Singleton
EGUsphere, https://doi.org/10.5194/egusphere-2024-1567, https://doi.org/10.5194/egusphere-2024-1567, 2024
Short summary
Short summary
At the high temperatures present in the deeper crust, minerals such as quartz can flow much like silly putty. The detailed mechanisms of how atoms are reorganized depends upon several factors, such as the temperature and the rate of which the mineral changes shape. We present observations from a naturally-deformed rock showing that the amount of water present also influences the type of deformation in quartz, with implications for geological interpretations.
Matthew S. Hodge, Guri Venvik, Jochen Knies, Roelant van der Lelij, Jasmin Schönenberger, Øystein Nordgulen, Marco Brönner, Aziz Nasuti, and Giulio Viola
Solid Earth, 15, 589–615, https://doi.org/10.5194/se-15-589-2024, https://doi.org/10.5194/se-15-589-2024, 2024
Short summary
Short summary
Smøla island, in the mid-Norwegian margin, has complex fracture and fault patterns resulting from tectonic activity. This study uses a multiple-method approach to unravel Smøla's tectonic history. We found five different phases of deformation related to various fracture geometries and minerals dating back hundreds of millions of years. 3D models of these features visualise these structures in space. This approach may help us to understand offshore oil and gas reservoirs hosted in the basement.
Pramit Chatterjee, Arnab Roy, and Nibir Mandal
EGUsphere, https://doi.org/10.5194/egusphere-2024-1077, https://doi.org/10.5194/egusphere-2024-1077, 2024
Short summary
Short summary
Understanding the strain accumulation processes in ductile shear zones is essential to explain the failure mechanisms at great crustal depths. This study explores the rheological and kinematic factors determining the varying modes of shear accommodation in natural shear zones. Numerical simulations suggest that an interplay of the following parameters: initial bulk viscosity, bulk shear rate, and internal cohesion governs the dominance of one accommodation mechanism over the other.
Karsten Reiter, Oliver Heidbach, and Moritz O. Ziegler
Solid Earth, 15, 305–327, https://doi.org/10.5194/se-15-305-2024, https://doi.org/10.5194/se-15-305-2024, 2024
Short summary
Short summary
It is generally assumed that faults have an influence on the stress state of the Earth’s crust. It is questionable whether this influence is still present far away from a fault. Simple numerical models were used to investigate the extent of the influence of faults on the stress state. Several models with different fault representations were investigated. The stress fluctuations further away from the fault (> 1 km) are very small.
Yukinojo Koyama, Simon R. Wallis, and Takayoshi Nagaya
Solid Earth, 15, 143–166, https://doi.org/10.5194/se-15-143-2024, https://doi.org/10.5194/se-15-143-2024, 2024
Short summary
Short summary
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.
Annelotte Weert, Kei Ogata, Francesco Vinci, Coen Leo, Giovanni Bertotti, Jerome Amory, and Stefano Tavani
Solid Earth, 15, 121–141, https://doi.org/10.5194/se-15-121-2024, https://doi.org/10.5194/se-15-121-2024, 2024
Short summary
Short summary
On the road to a sustainable planet, geothermal energy is considered one of the main substitutes when it comes to heating. The geological history of an area can have a major influence on the application of these geothermal systems, as demonstrated in the West Netherlands Basin. Here, multiple episodes of rifting and subsequent basin inversion have controlled the distribution of the reservoir rocks, thus influencing the locations where geothermal energy can be exploited.
Pâmela C. Richetti, Frank Zwaan, Guido Schreurs, Renata S. Schmitt, and Timothy C. Schmid
Solid Earth, 14, 1245–1266, https://doi.org/10.5194/se-14-1245-2023, https://doi.org/10.5194/se-14-1245-2023, 2023
Short summary
Short summary
The Araripe Basin in NE Brazil was originally formed during Cretaceous times, as South America and Africa broke up. The basin is an important analogue to offshore South Atlantic break-up basins; its sediments were uplifted and are now found at 1000 m height, allowing for studies thereof, but the cause of the uplift remains debated. Here we ran a series of tectonic laboratory experiments that show how a specific plate tectonic configuration can explain the evolution of the Araripe Basin.
Malte Froemchen, Ken J. W. McCaffrey, Mark B. Allen, Jeroen van Hunen, Thomas B. Phillips, and Yueren Xu
EGUsphere, https://doi.org/10.5194/egusphere-2023-2563, https://doi.org/10.5194/egusphere-2023-2563, 2023
Short summary
Short summary
The Shanxi Rift is a young active rift in North China that formed superimposed on a Proterozoic orogen. The impact of these structures on the active rift faults is poorly constrained. Here we quantify the landscape response to active faulting and compare these to published maps of inherited structures. We find that inherited structures played an important role in the segmentation of the Shanxi Rift and in the development of Rift Interaction Zones, the most active regions of the Shanxi Rift.
Adam J. Cawood, Hannah Watkins, Clare E. Bond, Marian J. Warren, and Mark A. Cooper
Solid Earth, 14, 1005–1030, https://doi.org/10.5194/se-14-1005-2023, https://doi.org/10.5194/se-14-1005-2023, 2023
Short summary
Short summary
Here we test conceptual models of fracture development by investigating fractures across multiple scales. We find that most fractures increase in abundance towards the fold hinge, and we interpret these as being fold related. Other fractures at the site show inconsistent orientations and are unrelated to fold formation. Our results show that predicting fracture patterns requires the consideration of multiple geologic variables.
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
Short summary
Short summary
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
Short summary
Short summary
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
Short summary
Short summary
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
Short summary
Short summary
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
Short summary
Short summary
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
Short summary
Short summary
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
Short summary
Short summary
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
Short summary
Short summary
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
Short summary
Short summary
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
Preprint archived
Short summary
Short summary
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
Short summary
Short summary
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
Short summary
Short summary
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
Short summary
Short summary
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
Short summary
Short summary
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
Short summary
Short summary
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
Short summary
Short summary
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
Short summary
Short summary
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
Short summary
Short summary
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
Short summary
Short summary
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
Short summary
Short summary
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
Short summary
Short summary
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
Short summary
Short summary
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
Short summary
Short summary
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
Short summary
Short summary
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
Short summary
Short summary
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
Short summary
Short summary
(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
Short summary
Short summary
Interpretation of newly acquired FRANKEN 2D seismic survey data in southeeastern Germany shows that upper Paleozoic low-grade metasedimentary rocks and possible nappe units are transported by Variscan shear zones to ca. 65 km west of the Franconian Fault System (FFS). We show that the locations of post-Variscan upper Carboniferous–Permian normal faults and associated graben and half-graben basins are controlled by the geometry of underlying Variscan shear zones.
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
Short summary
Short summary
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
Short summary
Short summary
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
Short summary
Short summary
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
Short summary
Short summary
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
Short summary
Short summary
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
Short summary
Short summary
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.
Chao Deng, Rixiang Zhu, Jianhui Han, Yu Shu, Yuxiang Wu, Kefeng Hou, and Wei Long
Solid Earth, 12, 2327–2350, https://doi.org/10.5194/se-12-2327-2021, https://doi.org/10.5194/se-12-2327-2021, 2021
Short summary
Short summary
This study uses seismic reflection data to interpret the geometric relationship and evolution of intra-basement and rift-related structures in the Enping sag in the northern South China Sea. Our observations suggest the primary control of pre-existing thrust faults is the formation of low-angle normal faults, with possible help from low-friction materials, and the significant role of pre-existing basement thrust faults in fault geometry, paleotopography, and syn-rift stratigraphy of rift basins.
Sonia Yeung, Marnie Forster, Emmanuel Skourtsos, and Gordon Lister
Solid Earth, 12, 2255–2275, https://doi.org/10.5194/se-12-2255-2021, https://doi.org/10.5194/se-12-2255-2021, 2021
Short summary
Short summary
We do not know when the ancient Tethys Ocean lithosphere began to founder, but one clue can be found in subduction accreted tectonic slices, including Gondwanan basement terranes on the island of Ios, Cyclades, Greece. We propose a 250–300 km southwards jump of the subduction megathrust with a period of flat-slab subduction followed by slab break-off. The initiation and its subsequent rollback of a new subduction zone would explain the onset of Oligo–Miocene extension and accompanying magmatism.
Rahul Prabhakaran, Giovanni Bertotti, Janos Urai, and David Smeulders
Solid Earth, 12, 2159–2209, https://doi.org/10.5194/se-12-2159-2021, https://doi.org/10.5194/se-12-2159-2021, 2021
Short summary
Short summary
Rock fractures are organized as networks with spatially varying arrangements. Due to networks' influence on bulk rock behaviour, it is important to quantify network spatial variation. We utilize an approach where fracture networks are treated as spatial graphs. By combining graph similarity measures with clustering techniques, spatial clusters within large-scale fracture networks are identified and organized hierarchically. The method is validated on a dataset with nearly 300 000 fractures.
Olivier Lacombe, Nicolas E. Beaudoin, Guilhem Hoareau, Aurélie Labeur, Christophe Pecheyran, and Jean-Paul Callot
Solid Earth, 12, 2145–2157, https://doi.org/10.5194/se-12-2145-2021, https://doi.org/10.5194/se-12-2145-2021, 2021
Short summary
Short summary
This paper aims to illustrate how the timing and duration of contractional deformation associated with folding in orogenic forelands can be constrained by the dating of brittle mesostructures observed in folded strata. The study combines new and already published absolute ages of fractures to provide, for the first time, an educated discussion about the factors controlling the duration of the sequence of deformation encompassing layer-parallel shortening, fold growth, and late fold tightening.
Vincent Famin, Hugues Raimbourg, Muriel Andreani, and Anne-Marie Boullier
Solid Earth, 12, 2067–2085, https://doi.org/10.5194/se-12-2067-2021, https://doi.org/10.5194/se-12-2067-2021, 2021
Short summary
Short summary
Sediments accumulated in accretionary prisms are deformed by the compression imposed by plate subduction. Here we show that deformation of the sediments transforms some minerals in them. We suggest that these mineral transformations are due to the proliferation of microorganisms boosted by deformation. Deformation-enhanced microbial proliferation may change our view of sedimentary and tectonic processes in subduction zones.
Cited articles
Angiboust, S., Agard, P., Raimbourg, H., Yamato, P. and Huet, B.: Subduction
interface processes recorded by eclogite-facies shear zones (Monviso, W.
Alps), Lithos, 127, 222–238, https://doi.org/10.1016/j.lithos.2011.09.004, 2011.
Ashby, M. and Verrall, R.: Diffusion-accommodated flow and
superplasticity, Acta Metall., 21, 149–163,
https://doi.org/10.1016/0001-6160(73)90057-6, 1973.
Austrheim, H.: Eclogitization of lower crustal granulites by fluid migration
through shear zones, Earth Planet. Sci. Lett., 81, 221–232,
https://doi.org/10.1016/0012-821X(87)90158-0, 1987.
Baratoux, L., Schulmann, K., Ulrich, S., and Lexa, O.: Contrasting
microstructures and deformation mechanisms in metagabbro mylonites
contemporaneously deformed under different temperatures (c. 650 C and c.
750 C), Geol. Soc. London, Spec. Publ., 243, 97–125,
https://doi.org/10.1144/GSL.SP.2005.243.01.09, 2005.
Barreiro, J. G., Lonardelli, I., Wenk, H. R., Dresen, G., Rybacki, E., Ren,
Y., and Tomé, C. N.: Preferred orientation of anorthite deformed
experimentally in Newtonian creep, Earth Planet. Sci. Lett., 264,
188–207, https://doi.org/10.1016/J.EPSL.2007.09.018, 2007.
Behrmann, J. H.: Crystal plasticity and superplasticity in quartzite; A
natural example, Tectonophysics, 115, 101–129,
https://doi.org/10.1016/0040-1951(85)90102-7, 1985.
Bell, D. R., Ihinger, P. D., and Rossman, G. R.: Quantitative analysis of
trace OH in garnet and pyroxenes, Am. Mineral., 80, 465–474,
https://doi.org/10.2138/am-1995-5-607, 1995.
Bercovici, D. and Ricard, Y.: Mechanisms for the generation of plate
tectonics by two-phase grain-damage and pinning, Phys. Earth Planet. Inter.,
202–203, 27–55, https://doi.org/10.1016/J.PEPI.2012.05.003, 2012.
Berger, A. and Stünitz, H.: Deformation mechanisms and reaction of
hornblende: examples from the Bergell tonalite (Central Alps),
Tectonophysics, 257, 149–174, https://doi.org/10.1016/0040-1951(95)00125-5,
1996.
Berthé, D., Choukroune, P., and Jegouzo, P.: Orthogneiss, mylonite and
non coaxial deformation of granites: the example of the South Armorican
Shear Zone, J. Struct. Geol., 1, 31–42,
https://doi.org/10.1016/0191-8141(79)90019-1, 1979.
Bons, P. D. and Den Brok, B.: Crystallographic preferred orientation
development by dissolution-precipitation creep, J. Struct.
Geol., 22, 1713–1722, 2000.
Borg, I. and Handin, J.: Experimental deformation of crystalline rocks,
Tectonophysics, 3, 249–367, https://doi.org/10.1016/0040-1951(66)90019-9, 1966.
Boullier, A. M. and Gueguen, Y.: SP-Mylonites: Origin of some mylonites by
superplastic flow, Contrib. Mineral. Petrol., 50, 93–104,
https://doi.org/10.1007/BF00373329, 1975.
Brander, L., Svahnberg, H., and Piazolo, S.: Brittle-plastic deformation in
initially dry rocks at fluid-present conditions: Transient behaviour of
feldspar at mid-crustal levels, Contrib. Mineral. Petrol., 163,
403–425, https://doi.org/10.1007/s00410-011-0677-5, 2012.
Brodie, K. H.: Variations in mineral chemistry across a shear zone in
phlogopite peridotite, J. Struct. Geol., 2, 265–272,
https://doi.org/10.1016/0191-8141(80)90059-0, 1980.
Brodie, K. H. and Rutter, E. H.: On the Relationship between Deformation and
Metamorphism, with Special Reference to the Behavior of Basic Rocks, pp.
138–179, Springer, New York, NY, 1985.
Brodie, K. H. and Rutter, E. H.: The role of transiently fine-grained
reaction products in syntectonic metamorphism: natural and experimental
examples, Can. J. Earth Sci., 24, 556–564, https://doi.org/10.1139/e87-054, 1987.
Brodie, K. H., Rutter, E. H., and Evans, P.: On the structure of the
Ivrea-Verbano Zone (northern Italy) and its implications for present-day
lower continental crust geometry, Terra Nov., 4, 34–40,
https://doi.org/10.1111/j.1365-3121.1992.tb00448.x, 1992.
Bunge, H.-J.: Texture analysis in materials science?: mathematical methods,
Butterworths, London, ISBN: 978-0-408-10642-9, 1982.
Bystricky, M. and Mackwell, S.: Creep of dry clinopyroxene aggregates, J.
Geophys. Res.-Solid Earth, 106, 13443–13454, https://doi.org/10.1029/2001JB000333,
2001.
Bystricky, M., Lawlis, J., Mackwell, S., Heidelbach, F., and Raterron, P.:
High-temperature deformation of enstatite aggregates, J. Geophys. Res.-Solid
Earth, 121, 6384–6400, https://doi.org/10.1002/2016JB013011, 2016.
Coe, R. S.: The thermodynamic effect of shear stress on the ortho-clino
inversion in enstatite and other coherent phase transitions characterized by
a finite simple shear, Contrib. Mineral. Petrol., 26, 247–264,
https://doi.org/10.1007/BF00373203, 1970.
Coe, R. S. and Kirby, S. H.: The orthoenstatite to clinoenstatite
transformation by shearing and reversion by annealing: Mechanism and
potential applications, Contrib. Mineral. Petrol., 52, 29–55,
https://doi.org/10.1007/BF00378000, 1975.
Connolly, J. A. D.: The geodynamic equation of state: What and how,
Geochemistry, Geophys. Geosystems, 10, Q10014,,
https://doi.org/10.1029/2009GC002540, 2009.
Dale, J., Powell, R., White, R. W., Elmer, F. L., and Holland, T. J. B.: A
thermodynamic model for Ca-Na clinoamphiboles in
Na2O-CaO-FeO-MgO-Al2O3-SiO2-H2O-O for petrological calculations, J.
Metamorph. Geol., 23, 771–791, https://doi.org/10.1111/j.1525-1314.2005.00609.x,
2005.
Degli Alessandrini, G., Menegon, L., Malaspina, N., Dijkstra, A. H., and
Anderson, M. W.: Creep of mafic dykes infiltrated by melt in the lower
continental crust (Seiland Igneous Province, Norway), Lithos, 274–275,
169–187, https://doi.org/10.1016/j.lithos.2016.12.030, 2017.
Dell'Angelo, L. N. and Tullis, J.: Textural and mechanical evolution with
progressive strain in experimentally deformed aplite, Tectonophysics,
256, 57–82, https://doi.org/10.1016/0040-1951(95)00166-2, 1996.
De Ronde, A. A. and Stünitz, H.: Deformation-enhanced reaction in
experimentally deformed plagioclase-olivine aggregates, Contrib. Mineral.
Petrol., 153, 699–717, https://doi.org/10.1007/s00410-006-0171-7, 2007.
De Ronde, A. A., Heilbronner, R., Stünitz, H., and Tullis, J.: Spatial
correlation of deformation and mineral reaction in experimentally deformed
plagioclase-olivine aggregates, Tectonophysics, 389, 93–109,
https://doi.org/10.1016/j.tecto.2004.07.054, 2004.
De Ronde, A. A., Stünitz, H., Tullis, J., and Heilbronner, R.:
Reaction-induced weakening of plagioclase-olivine composites,
Tectonophysics, 409, 85–106, https://doi.org/10.1016/j.tecto.2005.08.008, 2005.
Dimanov, A. and Dresen, G.: Rheology of synthetic anorthite-diopside
aggregates: Implications for ductile shear zones, J. Geophys. Res.-Solid
Earth, 110, 1–24, https://doi.org/10.1029/2004JB003431, 2005.
Dimanov, A., Lavie, M. P., Dresen, G., Ingrin, J., and Jaoul, O.: Creep of
polycrystalline anorthite and diopside, J. Geophys. Res.-Solid Earth,
108, 2061, https://doi.org/10.1029/2002JB001815, 2003.
Dimanov, A., Rybacki, E., Wirth, R., and Dresen, G.: Creep and
strain-dependent microstructures of synthetic anorthite–diopside
aggregates, J. Struct. Geol., 29, 1049–1069,
https://doi.org/10.1016/J.JSG.2007.02.010, 2007.
Elyaszadeh, R., Prior, D. J., Sarkarinejad, K., and Mansouri, H.: Different
slip systems controlling crystallographic preferred orientation and
intracrystalline deformation of amphibole in mylonites from the Neyriz
mantle diapir, Iran, J. Struct. Geol., 107, 38–52,
https://doi.org/10.1016/j.jsg.2017.11.020, 2018.
Etheridge, M. A., Wall, V. J., and Vernon, R. H.: The role of the fluid phase
during regional metamorphism and deformation, J. Metamorph. Geol., 1,
205–226, https://doi.org/10.1111/j.1525-1314.1983.tb00272.x, 1983.
Farla, R. J. M., Karato, S.-I., and Cai, Z.: Role of orthopyroxene in
rheological weakening of the lithosphere via dynamic recrystallization,
P. Natl. Acad. Sci. USA, 110, 16355–16360,
https://doi.org/10.1073/pnas.1218335110, 2013.
Fitz Gerald, J. and Stünitz, H.: Deformation of granitoids at low
m∼ tamo∼ ∼ ic grade. I: Reactions
and grain size reduction, Elsevier Sci. Publ. B.V, 221, 269–297,
https://doi.org/10.1016/0040-1951(93)90164-F, 1993.
Fliervoet, T. F. and White, S. H.: Quartz deformation in a very fine grained
quartzo-feldspathic mylonite: a lack of evidence for dominant grain boundary
sliding deformation, J. Struct. Geol., 17, 1095–1109,
https://doi.org/10.1016/0191-8141(95)00007-Z, 1995.
Fliervoet, T. F., White, S. H., and Drury, M. R.: Evidence for dominant
grain-boundary sliding deformation in greenschist- and amphibolite-grade
polymineralic ultramylonites from the Redbank Deformed Zone, Central
Australia, J. Struct. Geol., 19, 1495–1520,
https://doi.org/10.1016/S0191-8141(97)00076-X, 1997.
Fusseis, F., Regenauer-Lieb, K., Liu, J., Hough, R. M., and De Carlo, F.:
Creep cavitation can establish a dynamic granular fluid pump in ductile
shear zones, Nature, 459, 974–977, https://doi.org/10.1038/nature08051, 2009.
Gapais, D.: Shear structures within deformed granites: Mechanical and
thermal indicators, Geology, 17, 1144–1147, 1989.
Getsinger, A. J. and Hirth, G.: Amphibole fabric formation during diffusion
creep and the rheology of shear zones, Geology, 42, 535–538,
https://doi.org/10.1130/G35327.1, 2014.
Getsinger, A. J., Hirth, G., Stünitz, H., and Goergen, E. T.: Influence
of water on rheology and strain localization in the lower continental crust,
Geochem. Geophys. Geosy., 14, 2247–2264,
https://doi.org/10.1002/ggge.20148, 2013.
Gilgannon, J., Fusseis, F., Menegon, L., Regenauer-Lieb, K., and Buckman, J.: Hierarchical creep cavity formation in an ultramylonite and implications for phase mixing, Solid Earth, 8, 1193–1209, https://doi.org/10.5194/se-8-1193-2017, 2017.
Giuntoli, F., Menegon, L., and Warren, C. J.: Replacement reactions and
deformation by dissolution and precipitation processes in amphibolites, J.
Metamorph. Geol., 36, 1263–1286, https://doi.org/10.1111/jmg.12445, 2018.
Gueydan, F., Leroy, Y. M., and Jolivet, L.: Mechanics of low-angle
extensional shear zones at the brittle-ductile transition, J. Geophys. Res.-Solid Earth, 109, 1–16, https://doi.org/10.1029/2003JB002806, 2004.
Handy, M. R.: Flow laws for rocks containing two non-linear viscous phases:
A phenomenological approach, J. Struct. Geol., 16, 287–301,
https://doi.org/10.1016/0191-8141(94)90035-3, 1994.
Handy, M. R. and Stünitz, H.: Strain localization by fracturing and
reaction weakening – a mechanism for initiating exhumation of
subcontinental mantle beneath rifted margins, Geol. Soc. London, Spec.
Publ., 200, 387–407, https://doi.org/10.1144/GSL.SP.2001.200.01.22, 2002.
Harigane, Y., Michibayashi, K., and Ohara, Y.: Shearing within lower crust
during progressive retrogression: Structural analysis of gabbroic rocks from
the Godzilla Mullion, an oceanic core complex in the Parece Vela backarc
basin, Tectonophysics, 457, 183–196, https://doi.org/10.1016/j.tecto.2008.06.009,
2008.
Herwegh, M. and Berger, A.: Deformation mechanisms in second-phase affected
microstructures and their energy balance, J. Struct. Geol., 26,
1483–1498, https://doi.org/10.1016/J.JSG.2003.10.006, 2004.
Herwegh, M., Linckens, J., Ebert, A., Berger, A., and Brodhag, S. H.: The
role of second phases for controlling microstructural evolution in
polymineralic rocks: A review, J. Struct. Geol., 33, 1728–1750,
https://doi.org/10.1016/j.jsg.2011.08.011, 2011.
Holland, T. J. B. and Powell, R.: An internally consistent thermodynamic
data set for phases of petrological interest, J. Metamorph. Geol., 16,
309–343, https://doi.org/10.1111/j.1525-1314.1998.00140.x, 1998.
Holyoke, C. W. and Tullis, J.: Formation and maintenance of shear zones,
Geology, 34, 105–108, https://doi.org/10.1130/G22116.1, 2006a.
Holyoke, C. W. and Tullis, J.: Mechanisms of weak phase interconnection and
the effects of phase strength contrast on fabric development, J. Struct.
Geol., 28, 621–640, https://doi.org/10.1016/j.jsg.2006.01.008, 2006b.
Imon, R., Okudaira, T., and Fujimoto, A.: Dissolution and precipitation
processes in deformed amphibolites: an example from the ductile shear zone
of the Ryoke metamorphic belt, SW Japan, J. Metamorph. Geol., 20,
297–308, https://doi.org/10.1046/j.1525-1314.2002.00367.x, 2002.
Imon, R., Okudaira, T., and Kanagawa, K.: Development of shape- and
lattice-preferred orientations of amphibole grains during initial
cataclastic deformation and subsequent deformation by
dissolution-precipitation creep in amphibolites from the Ryoke metamorphic
belt, SW Japan, J. Struct. Geol., 26, 793–805,
https://doi.org/10.1016/j.jsg.2003.09.004, 2004.
Johnson, E. A.: Water in nominally anhydrous crustal minerals: Speciation,
concentration, and geologic significance, in: Water in Nominally Anhydrous
Minerals, vol. 62, pp. 117–154, Walter de Gruyter GmbH, 2006.
Johnson, E. A. and Rossmann, G. R.: The concentration and speciation of
hydrogen in feldspars using FTIR and 1H MAS NMR spectroscopy, Am. Mineral.,
88, 901–911, https://doi.org/10.2138/am-2003-5-620, 2003.
Johnson, E. A. and Rossman, G. R.: A survey of hydrous species and
concentrations in igneous feldspars, Am. Mineral., 89, 586–600,
https://doi.org/10.2138/am-2004-0413, 2004.
Jolivet, L. and Miyashita, S.: The Hidaka Shear Zone (Hokkaido, Japan):
Genesis during a right-lateral strike-slip movement, Tectonics, 4,
289–302, https://doi.org/10.1029/TC004i003p00289, 1985.
Jordan, P.: The rheology of polymineralic rocks - an approach, Geol.
Rundschau, 77, 285–294, https://doi.org/10.1007/BF01848690, 1988.
Kanagawa, K., Shimano, H., and Hiroi, Y.: Mylonitic deformation of gabbro in
the lower crust: A case study from the Pankenushi gabbro in the Hidaka
metamorphic belt of central Hokkaido, Japan, J. Struct. Geol., 30,
1150–1166, https://doi.org/10.1016/j.jsg.2008.05.007, 2008.
Keller, L. M., Abart, R., Stünitz, H., and De Capitani, C.: Deformation,
mass transfer and mineral reactions in an eclogite facies shear zone in a
polymetamorphic metapelite (Monte Rosa nappe, western Alps), J. Metamorph.
Geol., 22, 97–118, https://doi.org/10.1111/j.1525-1314.2004.00500.x, 2004.
Kenkmann, T. and Dresen, G.: Dislocation microstructure and phase
distribution in a lower crustal shear zone – An example from the Ivrea-Zone,
Italy, Int. J. Earth Sci., 91, 445–458, https://doi.org/10.1007/s00531-001-0236-9,
2002.
Kerrich, R., Allison, I., Barnett, R. L., Moss, S., and Starkey, J.:
Microstructural and chemical transformations accompanying deformation of
granite in a shear zone at Miéville, Switzerland; with implications for
stress corrosion cracking and superplastic flow, Contrib. Mineral.
Petrol., 73, 221–242, https://doi.org/10.1007/BF00381442, 1980.
Kilian, R., Heilbronner, R., and Stünitz, H.: Quartz grain size reduction
in a granitoid rock and the transition from dislocation to diffusion creep,
J. Struct. Geol., 33, 1265–1284, https://doi.org/10.1016/j.jsg.2011.05.004, 2011.
Knipe, R.: Deformation mechanisms – recognition from natural tectonites,
J. Struct. Geol., 11, 127–146, https://doi.org/10.1016/0191-8141(89)90039-4,
1989.
Kohlstedt, D. L., Evans, B., and Mackwell, S. J.: Strength of the
lithosphere: Constraints imposed by laboratory experiments, J. Geophys. Res.-Solid Earth, 100, 17587–17602, https://doi.org/10.1029/95JB01460, 1995.
Kruse, R. and Stünitz, H.: Deformation mechanisms and phase distribution
in mafic high-temperature mylonites from the Jotun Nappe, southern Norway,
Tectonophysics, 303, 223–249, https://doi.org/10.1016/S0040-1951(98)00255-8,
1999.
Langdon, T. G.: Grain boundary sliding revisited: Developments in sliding
over four decades, J. Mater. Sci., 41, 597–609,
https://doi.org/10.1007/s10853-006-6476-0, 2006.
Linckens, J., Herwegh, M., Müntener, O., and Mercolli, I.: Evolution of a
polymineralic mantle shear zone and the role of second phases in the
localization of deformation, J. Geophys. Res.-Solid Earth, 116, B06210,
https://doi.org/10.1029/2010JB008119, 2011.
Linckens, J., Herwegh, M., and Müntener, O.: Small quantity but large
effect - How minor phases control strain localization in upper mantle shear
zones, Tectonophysics, 643, 26–43, https://doi.org/10.1016/j.tecto.2014.12.008, 2015.
Mansard, N., Raimbourg, H., Augier, R., Précigout, J., and Le Breton, N.:
Large-scale strain localization induced by phase nucleation in mid-crustal
granitoids of the south Armorican massif, Tectonophysics, 745,
https://doi.org/10.1016/j.tecto.2018.07.022, 2018.
Mansard, N., Stünitz, H., Raimbourg, H., and Précigout, J.: The role
of deformation-reaction interactions to localize strain in polymineralic
rocks: Insights from experimentally deformed plagioclase-pyroxene
assemblages, J. Struct. Geol., 134, 104008, https://doi.org/10.1016/j.jsg.2020.104008, 2020.
Marti, S., Stünitz, H., Heilbronner, R., Plümper, O., and Drury, M.:
Experimental investigation of the brittle-viscous transition in mafic rocks
– Interplay between fracturing, reaction, and viscous deformation, J.
Struct. Geol., 105, 62–79, https://doi.org/10.1016/j.jsg.2017.10.011, 2017.
Marti, S., Stünitz, H., Heilbronner, R., Plümper, O., and Kilian, R.: Syn-kinematic hydration reactions, grain size reduction, and dissolution–precipitation creep in experimentally deformed plagioclase–pyroxene mixtures, Solid Earth, 9, 985–1009, https://doi.org/10.5194/se-9-985-2018, 2018.
Mehl, L. and Hirth, G.: Plagioclase preferred orientation in layered
mylonites: Evaluation of flow laws for the lower crust, J. Geophys. Res.,
113, B05202, https://doi.org/10.1029/2007JB005075, 2008.
Menegon, L., Fusseis, F., Stünitz, H., and Xiao, X.: Creep cavitation
bands control porosity and fluid flow in lower crustal shear zones, Geology,
43, 227–230, https://doi.org/10.1130/G36307.1, 2015.
Miyazaki, T., Sueyoshi, K., and Hiraga, T.: Olivine crystals align during
diffusion creep of Earth's upper mantle, Nature, 502, 321–326,
https://doi.org/10.1038/nature12570, 2013.
Montési, L. G. J.: Fabric development as the key for forming ductile
shear zones and enabling plate tectonics, J. Struct. Geol., 50, 254–266,
https://doi.org/10.1016/j.jsg.2012.12.011, 2013.
Newman, J., Lamb, W. M., Drury, M. R., and Vissers, R. L. M.: Deformation
processes in a peridotite shear zone: reaction-softening by an
H2O-deficient, continuous net transfer reaction, Tectonophysics, 303,
193–222, https://doi.org/10.1016/S0040-1951(98)00259-5, 1999.
Newton, R. C.: Fluids and shear zones in the deep crust, Tectonophysics,
182, 21–37, https://doi.org/10.1016/0040-1951(90)90339-A, 1990.
Newton, R. C., Charlu, T. V., and Kleppa, O. J.: Thermochemistry of the high
structural state plagioclases, Geochim. Cosmochim. Acta, 44, 933–941,
https://doi.org/10.1016/0016-7037(80)90283-5, 1980.
Nicolas, A. and Christensen, N. I.: Formation of anisotropy in upper mantle
peridotites: A review, pp. 111–123, American Geophysical Union (AGU),
1987.
Okudaira, T., Jeřábek, P., Stünitz, H., and Fusseis, F.:
High-temperature fracturing and subsequent grain-size-sensitive creep in
lower crustal gabbros: Evidence for coseismic loading followed by creep
during decaying stress in the lower crust, J. Geophys. Res.-Solid Earth,
120, 3119–3141, https://doi.org/10.1002/2014JB011708, 2015.
Okudaira, T., Shigematsu, N., Harigane, Y., and Yoshida, K.: Grain size
reduction due to fracturing and subsequent grain-size-sensitive creep in a
lower crustal shear zone in the presence of a CO2-bearing fluid, J. Struct.
Geol., 95, 171–187, https://doi.org/10.1016/j.jsg.2016.11.001, 2017.
Olgaard, D. L.: The role of second phase in localizing deformation, Geol.
Soc. London, Spec. Publ., 54, 175–181,
https://doi.org/10.1144/GSL.SP.1990.054.01.17, 1990.
Olgaard, D. L. and Evans, B.: Effect of Second-Phase Particles on Grain
Growth in Calcite, J. Am. Ceram. Soc., 69, C-272–C-277,
https://doi.org/10.1111/j.1151-2916.1986.tb07374.x, 1986.
Olgaard, D. L. and Evans, B.: Grain growth in synthetic marbles with added
mica and water, Contrib. Mineral. Petrol., 100, 246–260,
https://doi.org/10.1007/BF00373591, 1988.
Oliot, E., Goncalves, P., Schulmann, K., Marquer, D., and Lexa, O.:
Mid-crustal shear zone formation in granitic rocks: Constraints from
quantitative textural and crystallographic preferred orientations analyses,
Tectonophysics, 612–613, 63–80, https://doi.org/10.1016/j.tecto.2013.11.032, 2014.
Palazzin, G., Raimbourg, H., Stünitz, H., Heilbronner, R., Neufeld, K.,
and Précigout, J.: Evolution in H2O contents during deformation of
polycrystalline quartz: An experimental study, J. Struct. Geol., 114,
95–110, https://doi.org/10.1016/J.JSG.2018.05.021, 2018.
Paterson, M. S.: The determination of hydroxyl by infrared adsorption in
quartz, silicate glasses and similar materials., Bull. Mineral., 105,
20–29, https://doi.org/10.3406/bulmi.1982.7582, 1982.
Paterson, M. S.: Superplasticity in Geological Materials, MRS Proc., 196, 303,
https://doi.org/10.1557/proc-196-303, 1990.
Paterson, M. S.: A Granular Flow Approach to Fine-Grain Superplasticity, in:
Plastic Deformation of Ceramics, pp. 279–283, Springer USA, 1995.
Paterson, M. S.: Materials Science for Structural Geology, 1st ed.,
Springer, New York, 2013.
Pec, M., Stünitz, H., Heilbronner, R., Drury, M., and de Capitani, C.:
Origin of pseudotachylites in slow creep experiments, Earth Planet. Sci.
Lett., 355–356, 299–310, https://doi.org/10.1016/J.EPSL.2012.09.004, 2012a.
Pec, M., Stünitz, H., and Heilbronner, R.: Semi-brittle deformation of
granitoid gouges in shear experiments at elevated pressures and
temperatures, 38, 200–221, https://doi.org/10.1016/j.jsg.2011.09.001, 2012b.
Pec, M., Stünitz, H., Heilbronner, R., and Drury, M.: Semi-brittle flow
of granitoid fault rocks in experiments, J. Geophys. Res.-Solid Earth,
121, 1677–1705, https://doi.org/10.1002/2015JB012513, 2016.
Philippot, P. and Kienast, J. R.: Chemical-microstructural changes in
eclogite-facies shear zones (Monviso, Western Alps, north Italy) as
indicators of strain history and the mechanism and scale of mass transfer,
Lithos, 23, 179–200, https://doi.org/10.1016/0024-4937(89)90004-2, 1989.
Platt, J. P.: Rheology of two-phase systems: A microphysical and
observational approach, J. Struct. Geol., 77, 213–227,
https://doi.org/10.1016/j.jsg.2015.05.003, 2015.
Plümper, O., Botan, A., Los, C., Liu, Y., Malthe-Sørenssen, A., and
Jamtveit, B.: Fluid-driven metamorphism of the continental crust governed by
nanoscale fluid flow, Nat. Geosci., 10, 685–690, https://doi.org/10.1038/ngeo3009,
2017.
Powell, R. and Holland, T.: Relating formulations of the thermodynamics of
mineral solid solutions: Activity modeling of pyroxenes, amphiboles, and
micas, Am. Mineral., 84, 1–14, https://doi.org/10.2138/am-1999-1-201, 1999.
Précigout, J. and Hirth, G.: B-type olivine fabric induced by grain
boundary sliding, Earth Planet. Sci. Lett., 395, 231–240,
https://doi.org/10.1016/j.epsl.2014.03.052, 2014.
Précigout, J. and Stünitz, H.: Evidence of phase nucleation during
olivine diffusion creep: A new perspective for mantle strain localisation,
Earth Planet. Sci. Lett., 455, 94–105,
https://doi.org/10.1016/j.epsl.2016.09.029, 2016.
Précigout, J., Prigent, C., Palasse, L., and Pochon, A.: Water pumping in
mantle shear zones, Nat. Commun., 8, 15736, https://doi.org/10.1038/ncomms15736, 2017.
Précigout, J., Stünitz, H., Pinquier, Y., Champallier, R., and
Schubnel, A.: High-pressure, High-temperature Deformation Experiment Using
the New Generation Griggs-type Apparatus, J. Vis. Exp., 134, e56841,
https://doi.org/10.3791/56841, 2018.
Raimbourg, H., Toyoshima, T., Harima, Y., and Kimura, G.: Grain-size
reduction mechanisms and rheological consequences in high-temperature gabbro
mylonites of Hidaka, Japan, Earth Planet. Sci. Lett., 267, 637–653,
https://doi.org/10.1016/j.epsl.2007.12.012, 2008.
Richter, B., Stünitz, H., and Heilbronner, R.: The brittle-to-viscous
transition in polycrystalline quartz: An experimental study, J. Struct.
Geol., 114, 1–21, https://doi.org/10.1016/j.jsg.2018.06.005, 2018.
Rubie, D. C.: Reaction-enhanced ductility: The role of solid-solid
univariant reactions in deformation of the crust and mantle, Tectonophysics,
96, 331–352, https://doi.org/10.1016/0040-1951(83)90225-1, 1983.
Rudnick, R. L. and Fountain, D. M.: Nature and composition of the
continental crust: A lower crustal perspective, Rev. Geophys., 33, 267,
https://doi.org/10.1029/95RG01302, 1995.
Rutter, E. H. and Brodie, K. H.: The Permeation of Water into Hydrating
Shear Zones, Adv. Phys. Geochem., 4, 242–250, 1985.
Schmid, S. M.: Microfabric studies as indicators of deformation mechanisms
and flow laws operative in mountain building, Mt. Build. Process., edited by: Hsu, K. J., Academic Press,
95–110, 1982.
Schroeder, T. and John, B. E.: Strain localization on an oceanic detachment
fault system, Atlantis Massif, 30∘ N, Mid-Atlantic Ridge,
Geochem. Geophy. Geosy., 5, Q11007, https://doi.org/10.1029/2004GC000728, 2004.
Selverstone, J., Morteani, G., and Staude, J.-M.: Fluid channelling during
ductile shearing: transformation of granodiorite into aluminous schist in
the Tauern Window, Eastern Alps, J. Metamorph. Geol., 9, 419–431,
https://doi.org/10.1111/j.1525-1314.1991.tb00536.x, 1991.
Shelley, D.: Spider texture and amphibole preferred orientations, J. Struct.
Geol., 16, 709–717, https://doi.org/10.1016/0191-8141(94)90120-1, 1994.
Skemer, P., Katayama, I., Jiang, Z., and Karato, S.: The misorientation
index: Development of a new method for calculating the strength of
lattice-preferred orientation, Tectonophysics, 411, 157–167,
https://doi.org/10.1016/J.TECTO.2005.08.023, 2005.
Skogby, H.: Water in natural mantle minerals I: Pyroxenes, in: Water in
Nominally Anhydrous Minerals, vol. 62, pp. 155–168, Walter de Gruyter
GmbH, 2006.
Soret, M., Agard, P., Ildefonse, B., Dubacq, B., Prigent, C., and Rosenberg, C.: Deformation mechanisms in mafic amphibolites and granulites: record from the Semail metamorphic sole during subduction infancy, Solid Earth, 10, 1733–1755, https://doi.org/10.5194/se-10-1733-2019, 2019.
Stünitz, H. and Fitz Gerald, J. D.: Deformation of granitoids at low
metamorphic grades: II. Granular flow in albite rich mylonites,
Tectonophysics, 221, 299–324, https://doi.org/10.1016/0040-1951(93)90164-F, 1993.
Stünitz, H. and Tullis, J.: Weakening and strain localization produced
by syn-deformational reaction of plagioclase, Int. J. Earth Sci., 90,
136–148, https://doi.org/10.1007/s005310000148, 2001.
Sundberg, M. and Cooper, R. F.: Crystallographic preferred orientation
produced by diffusional creep of harzburgite: Effects of chemical
interactions among phases during plastic flow, J. Geophys. Res.-Solid Earth,
113, B12208, https://doi.org/10.1029/2008JB005618, 2008.
Svahnberg, H. and Piazolo, S.: Interaction of chemical and physical
processes during deformation at fluid-present conditions: A case study from
an anorthosite-leucogabbro deformed at amphibolite facies conditions,
Contrib. Mineral. Petrol., 165, 543–562,
https://doi.org/10.1007/s00410-012-0822-9, 2013.
Tasaka, M., Zimmerman, M. E., and Kohlstedt, D. L.: Evolution of the
rheological and microstructural properties of olivine aggregates during
dislocation creep under hydrous conditions, J. Geophys. Res.-Solid Earth,
121, 92–113, https://doi.org/10.1002/2015JB012134, 2016.
Tasaka, M., Zimmerman, M. E., Kohlstedt, D. L., Stünitz, H., and
Heilbronner, R.: Rheological Weakening of Olivine + Orthopyroxene
Aggregates Due To Phase Mixing: Part 2. Microstructural Development, J.
Geophys. Res.-Solid Earth, 122, 7597–7612, https://doi.org/10.1002/2017JB014311,
2017.
Tullis, J., Yund, R., and Farver, J.: Deformation-enhanced fluid distribution
in feldspar aggregates and implications for ductile shear zones, Geology,
24, 63–66, https://doi.org/10.1130/0091-7613(1996)024<0063:defdif>2.3.co;2, 1996.
Vissers, R. L. M., Drury, M. R., Newman, J., and Fliervoet, T. F.: Mylonitic
deformation in upper mantle peridotites of the North Pyrenean Zone (France):
implications for strength and strain localization in the lithosphere,
Tectonophysics, 279, 303–325, https://doi.org/10.1016/S0040-1951(97)00128-5,
1997.
Warren, J. M. and Hirth, G.: Grain size sensitive deformation mechanisms in
naturally deformed peridotites, Earth Planet. Sci. Lett., 248,
423–435, https://doi.org/10.1016/j.epsl.2006.06.006, 2006.
Wenk, H.-R. and Christie, J. M.: Comments on the interpretation of
deformation textures in rocks, J. Struct. Geol., 13, 1091–1110,
https://doi.org/10.1016/0191-8141(91)90071-P, 1991.
Wheeler, J.: Importance of pressure solution and coble creep in the
deformation of polymineralic rocks, J. Geophys. Res., 97, 4579,
https://doi.org/10.1029/91JB02476, 1992.
Short summary
Our rock deformation experiments (solid-medium Griggs-type apparatus) on wet assemblages of mafic compositions show that the ability of minerals to react controls the portions of rocks that deform and that minor chemical and mineralogical variations can considerably modify the strength of deformed assemblages. Our study suggests that the rheology of mafic rocks, which constitute a large part of the oceanic crust, cannot be summarized as being rheologically controlled by monophase materials.
Our rock deformation experiments (solid-medium Griggs-type apparatus) on wet assemblages of...