Olivine Grain Size Distributions in Faults and Shear Zones: Evidence for Nonsteady State Deformation-Reference-Cited by-同舟云学术

Olivine Grain Size Distributions in Faults and Shear Zones: Evidence for Nonsteady State Deformation

Published:2018-09 Issue:9 Volume:123 Page:7421-7443
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Aupart Claire¹^ORCID,Dunkel Kristina G.¹^ORCID,Angheluta Luiza²^ORCID,Austrheim Håkon¹^ORCID,Ildefonse Benoit³^ORCID,Malthe-Sørenssen Anders²^ORCID,Jamtveit Bjørn¹^ORCID

Affiliation:

1. Physics of Geological Processes, The Njord Centre, Department of Geosciences; University of Oslo; Oslo Norway

2. Physics of Geological Processes, The Njord Centre, Department of Physics; University of Oslo; Oslo Norway

3. Géosciences Montpellier, CNRS, University of Montpellier, Université des Antilles; Montpellier France

Funder

European Union's Horizon 2020 Research and Innovation Programme

ERC Advanced

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1029/2018JB015836/fullpdf

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3. Paleowattmeters: A scaling relation for dynamically recrystallized grain size;Austin;Geology,2007

4. Fragmentation of wall rock garnets during deep crustal earthquakes;Austrheim;Science Advances,2017

5. Garnets recording deep crustal earthquakes;Austrheim;Earth and Planetary Science Letters,1996

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