In:
Journal of Geophysical Research: Solid Earth, American Geophysical Union (AGU), Vol. 122, No. 5 ( 2017-05), p. 3895-3915
Abstract:
Fault microstructures record fast (seismic) to slow (aseismic) deformation stages consistent with some geophysical observations A few % of clays in natural fault gouge may strongly affect frictional behavior Shear experiments suggest that clay‐bearing layers have shorter weakening distance than carbonate‐pure gouges during seismic slip
Type of Medium:
Online Resource
ISSN:
2169-9313
,
2169-9356
DOI:
10.1002/2017JB014042
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2017
detail.hit.zdb_id:
2016813-5
detail.hit.zdb_id:
161666-3
detail.hit.zdb_id:
3094197-0
SSG:
16,13
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