Semi-brittle flow of granitoid fault rocks in experiments-Reference-Cited by-同舟云学术

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Semi-brittle flow of granitoid fault rocks in experiments

Published:2016-03 Issue:3 Volume:121 Page:1677-1705
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Pec Matej¹²,Stünitz Holger³⁴,Heilbronner Renée¹,Drury Martyn⁵

Affiliation:

1. Geological Institute; Basel University; Basel Switzerland

2. Department of Earth Sciences; University of Minnesota, Twin Cities; Minneapolis USA

3. Department of Geology; Tromsø University; Tromsø Norway

4. Institut des Sciences de la Terre d'Orléans; Université d'Orléans; Orléans France

5. Department of Earth Sciences; Utrecht University; Utrecht Netherlands

Funder

Swiss National Fonds

Publisher

American Geophysical Union (AGU)

Subject

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

Reference99 articles.

1. Deformation mechanisms and rheology of serpentines in experiments and in nature;Amiguet;J. Geophys. Res. Solid Earth,2014

2. The instantaneous rate dependence in low temperature laboratory rock friction and rock deformation experiments;Beeler;J. Geophys. Res.,2007

3. Fault stability inferred from granite sliding experiments at hydrothermal conditions;Blanpied;Geophys. Res. Lett.,1991

4. Frictional slip of granite at hydrothermal conditions;Blanpied;J. Geophys. Res.,1995

5. Quantitative measure of the variation in fault rheology due to fluid-rock interactions;Blanpied;J. Geophys. Res.,1998

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