Phase transformation and nanometric flow cause extreme weakening during fault slip

Nature Geoscience

Volumn 8, Issue 6, 2015, Pages 448-489

  Green, H W ^a   Shi, F ^a,b   Bozhilov, K ^a   Xia, G ^a,d   Reches, Z ^c  

^a UNIVERSITY OF CALIFORNIA   (United States)

^b CHINA UNIVERSITY OF GEOSCIENCES   (China)

^c UNIVERSITY OF OKLAHOMA   (United States)

^d UNIVERSITY OF QUEENSLAND   (Australia)

Author keywords

[No Author keywords available]

Indexed keywords

AUREOLE; EARTHQUAKE INTENSITY; EXTREME EVENT; FAULT SLIP; FAULTING; GRAIN BOUNDARY; INSTABILITY; SAN ANDREAS FAULT; SHEAR STRESS; TEMPERATURE GRADIENT;

EID: 84987838012     PISSN: 17520894     EISSN: 17520908     Source Type: Journal    
DOI: 10.1038/NGEO2436     Document Type: Article

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