Absence of Stress-Induced Anisotropy During Brittle Deformation in Antigorite Serpentinite

Author:

David Emmanuel C.1ORCID,Brantut Nicolas1ORCID,Hansen Lars N.2ORCID,Mitchell Thomas M.1ORCID

Affiliation:

1. Department of Earth Sciences; University College London; London UK

2. Department of Earth Sciences; University of Oxford; Oxford UK

Funder

Natural Environment Research Council

Publisher

American Geophysical Union (AGU)

Subject

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

Reference67 articles.

1. Creep of phyllosilicates at the onset of plate tectonics;Amiguet;Earth and Planetary Science Letters,2012

2. Deformation mechanisms of antigorite serpentinite at subduction zone conditions determined from experimentally and naturally deformed rocks;Auzende;Earth and Planetary Science Letters,2015

3. Critique of explicit schemes for estimating elastic properties of multiphase composites;Berryman;Mechanics of Materials,2002

4. Elasticity of antigorite, seismic detection of serpentinites, and anisotropy in subduction zones;Bezacier;Earth and Planetary Science Letters,2010

5. High-pressure elasticity of serpentine and seismic properties of the hydrated mantle wedge;Bezacier;Journal of Geophysical Research: Solid Earth,2013

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