Articles | Volume 9, issue 4
https://doi.org/10.5194/se-9-985-2018
© Author(s) 2018. 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-9-985-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
09 Aug 2018
Research article |
| 09 Aug 2018
| 09 Aug 2018
Syn-kinematic hydration reactions, grain size reduction, and dissolution–precipitation creep in experimentally deformed plagioclase–pyroxene mixtures
Sina Marti
CORRESPONDING AUTHOR
Department of Environmental Sciences, University of Basel, Basel, Switzerland
Holger Stünitz
Department of Geosciences, University of Tromsø, Tromsø, Norway
Institut des Sciences de la Terre d'Orléans (ISTO), Université d'Orléans, Orléans, France
Renée Heilbronner
Department of Environmental Sciences, University of Basel, Basel, Switzerland
Oliver Plümper
Department of Earth Sciences, Utrecht University, Utrecht, the Netherlands
Rüdiger Kilian
Department of Environmental Sciences, University of Basel, Basel, Switzerland
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Cited
26 citations as recorded by crossref.
- Dissolution precipitation creep as a process for the strain localisation in mafic rocks A. Lee et al. 10.1016/j.jsg.2021.104505
- Contribution of deformation and reaction of amphiboles to the weakening of the middle continental crust: A case study from sheared diorites along the Shuiyu shear zone in Northern Beijing H. Shan et al. 10.1016/j.jsg.2022.104727
- Thermometry and Microstructural Analysis Imply Protracted Extensional Exhumation of the Tso Morari UHP Nappe, Northwestern Himalaya: Implications for Models of UHP Exhumation S. Long et al. 10.1029/2020TC006482
- Strain localization at brittle-ductile transition depths during Miocene magmatism and exhumation in the southern Basin and Range A. Zuza et al. 10.1016/j.jsg.2022.104709
- Transformation weakening: Diffusion creep in eclogites as a result of interaction of mineral reactions and deformation H. Stünitz et al. 10.1016/j.jsg.2020.104129
- How Does Viscosity Contrast Influence Phase Mixing and Strain Localization? A. Cross et al. 10.1029/2020JB020323
- Grain boundary networks and shape preferred orientation – A fresh angle on pattern quantification with GBPaQ J. Heeb et al. 10.1016/j.cageo.2023.105311
- Deformation of mafic schists from subducted oceanic crust at high pressure and temperature conditions K. Okazaki & G. Hirth 10.1016/j.tecto.2019.228217
- Interplay between crystal-plasticity, fracturing and dissolution-precipitation creep in lower-crustal ultramylonite from hole U1473A, Atlantis Bank, Southwest Indian Ridge R. Taufner et al. 10.1016/j.jsg.2022.104780
- Numerical Simulations Reproduce Field Observations Showing Transient Weakening During Shear Zone Formation by Diffusional Hydrogen Influx and H2O Inflow L. Kaatz et al. 10.1029/2022GC010830
- The effect of strain on the crystallinity of carbonaceous matter: Application of Raman spectroscopy to deformation experiments B. Moris-Muttoni et al. 10.1016/j.tecto.2023.230126
- Crystal preferred orientations, deformation mechanisms and seismic properties of high pressure metamorphic rocks from the Central Qiangtang metamorphic belt, Tibetan Plateau Y. Cao et al. 10.1016/j.jsg.2021.104309
- Relationship between microstructures and resistance in mafic assemblages that deform and transform N. Mansard et al. 10.5194/se-11-2141-2020
- Fluid inclusion induced hardening: nanoscale evidence from naturally deformed pyrite R. Dubosq et al. 10.1007/s00410-021-01774-9
- Petrology of Palaeoarchaean mafic–ultramafic rock suites of the western Iron Ore Group, Singhbhum Craton, eastern India, using the chemistry of minerals M. Paul et al. 10.1017/S0016756822001170
- Deformation mechanisms of granulite-facies mafic shear zones from hole U1473A, Atlantis Bank, Southwest Indian Ridge (IODP Expedition 360) R. Taufner et al. 10.1016/j.jsg.2021.104380
- Transient weakening during the granulite to eclogite transformation within hydrous shear zones (Holsnøy, Norway) E. Bras et al. 10.1016/j.tecto.2021.229026
- Omphacite breakdown: nucleation and deformation of clinopyroxene-plagioclase symplectites S. Zertani et al. 10.1007/s00410-024-02125-0
- Slabitization: Mechanisms controlling subduction development and viscous coupling P. Agard et al. 10.1016/j.earscirev.2020.103259
- Rheology of continental lithosphere and seismic anisotropy S. Sun et al. 10.1007/s11430-022-1171-3
- Fluid-assisted dissolution-precipitation creep of garnet: An example from garnet-sillimanite gneiss in the Red River-Ailao Shan shear zone J. Lei et al. 10.18654/1000-0569/2021.02.11
- Amorphous material in experimentally deformed mafic rock and its temperature dependence: Implications for fault rheology during aseismic creep and seismic rupture S. Marti et al. 10.1016/j.jsg.2020.104081
- Diffusion Creep of Sodic Amphibole‐Bearing Blueschist Limited by Microboudinage L. Tokle et al. 10.1029/2023JB026848
- Interphase misorientation as a tool to study metamorphic reactions and crystallization in geological materials L. Morales 10.2138/am-2021-7902
- Enhancement of ductile deformation in polycrystalline anorthite due to the addition of water J. Fukuda et al. 10.1016/j.jsg.2022.104547
- Deformation mechanisms in mafic amphibolites and granulites: record from the Semail metamorphic sole during subduction infancy M. Soret et al. 10.5194/se-10-1733-2019
26 citations as recorded by crossref.
- Dissolution precipitation creep as a process for the strain localisation in mafic rocks A. Lee et al. 10.1016/j.jsg.2021.104505
- Contribution of deformation and reaction of amphiboles to the weakening of the middle continental crust: A case study from sheared diorites along the Shuiyu shear zone in Northern Beijing H. Shan et al. 10.1016/j.jsg.2022.104727
- Thermometry and Microstructural Analysis Imply Protracted Extensional Exhumation of the Tso Morari UHP Nappe, Northwestern Himalaya: Implications for Models of UHP Exhumation S. Long et al. 10.1029/2020TC006482
- Strain localization at brittle-ductile transition depths during Miocene magmatism and exhumation in the southern Basin and Range A. Zuza et al. 10.1016/j.jsg.2022.104709
- Transformation weakening: Diffusion creep in eclogites as a result of interaction of mineral reactions and deformation H. Stünitz et al. 10.1016/j.jsg.2020.104129
- How Does Viscosity Contrast Influence Phase Mixing and Strain Localization? A. Cross et al. 10.1029/2020JB020323
- Grain boundary networks and shape preferred orientation – A fresh angle on pattern quantification with GBPaQ J. Heeb et al. 10.1016/j.cageo.2023.105311
- Deformation of mafic schists from subducted oceanic crust at high pressure and temperature conditions K. Okazaki & G. Hirth 10.1016/j.tecto.2019.228217
- Interplay between crystal-plasticity, fracturing and dissolution-precipitation creep in lower-crustal ultramylonite from hole U1473A, Atlantis Bank, Southwest Indian Ridge R. Taufner et al. 10.1016/j.jsg.2022.104780
- Numerical Simulations Reproduce Field Observations Showing Transient Weakening During Shear Zone Formation by Diffusional Hydrogen Influx and H2O Inflow L. Kaatz et al. 10.1029/2022GC010830
- The effect of strain on the crystallinity of carbonaceous matter: Application of Raman spectroscopy to deformation experiments B. Moris-Muttoni et al. 10.1016/j.tecto.2023.230126
- Crystal preferred orientations, deformation mechanisms and seismic properties of high pressure metamorphic rocks from the Central Qiangtang metamorphic belt, Tibetan Plateau Y. Cao et al. 10.1016/j.jsg.2021.104309
- Relationship between microstructures and resistance in mafic assemblages that deform and transform N. Mansard et al. 10.5194/se-11-2141-2020
- Fluid inclusion induced hardening: nanoscale evidence from naturally deformed pyrite R. Dubosq et al. 10.1007/s00410-021-01774-9
- Petrology of Palaeoarchaean mafic–ultramafic rock suites of the western Iron Ore Group, Singhbhum Craton, eastern India, using the chemistry of minerals M. Paul et al. 10.1017/S0016756822001170
- Deformation mechanisms of granulite-facies mafic shear zones from hole U1473A, Atlantis Bank, Southwest Indian Ridge (IODP Expedition 360) R. Taufner et al. 10.1016/j.jsg.2021.104380
- Transient weakening during the granulite to eclogite transformation within hydrous shear zones (Holsnøy, Norway) E. Bras et al. 10.1016/j.tecto.2021.229026
- Omphacite breakdown: nucleation and deformation of clinopyroxene-plagioclase symplectites S. Zertani et al. 10.1007/s00410-024-02125-0
- Slabitization: Mechanisms controlling subduction development and viscous coupling P. Agard et al. 10.1016/j.earscirev.2020.103259
- Rheology of continental lithosphere and seismic anisotropy S. Sun et al. 10.1007/s11430-022-1171-3
- Fluid-assisted dissolution-precipitation creep of garnet: An example from garnet-sillimanite gneiss in the Red River-Ailao Shan shear zone J. Lei et al. 10.18654/1000-0569/2021.02.11
- Amorphous material in experimentally deformed mafic rock and its temperature dependence: Implications for fault rheology during aseismic creep and seismic rupture S. Marti et al. 10.1016/j.jsg.2020.104081
- Diffusion Creep of Sodic Amphibole‐Bearing Blueschist Limited by Microboudinage L. Tokle et al. 10.1029/2023JB026848
- Interphase misorientation as a tool to study metamorphic reactions and crystallization in geological materials L. Morales 10.2138/am-2021-7902
- Enhancement of ductile deformation in polycrystalline anorthite due to the addition of water J. Fukuda et al. 10.1016/j.jsg.2022.104547
- Deformation mechanisms in mafic amphibolites and granulites: record from the Semail metamorphic sole during subduction infancy M. Soret et al. 10.5194/se-10-1733-2019
Discussed (final revised paper)
Discussed (preprint)
Latest update: 23 Apr 2024
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.
Using rock deformation experiments we study how rocks deform at mid-crustal levels within...
