Shear Zone Evolution
Shear Zone Evolution is a geological process that describes the progressive development and transformation of a localized region of intense ductile to brittle deformation within the Earth's crust or mantle, distinguished by time-dependent changes in strain, fabric, geometry, and kinematics in response to tectonic forces.
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Dilatant strengthening as a mechanism for slow slip events
P. Segall, Allan M. Rubin, Andrew Bradley et al. · Journal of Geophysical Research Atmospheres · 2010 · 437 citations · Full text
Intraplate extension prior to continental extrusion along the Ailao Shan-Red River shear zone
Sun‐Lin Chung, Tung‐Yi Lee, Ching‐Hua Lo et al. · Geology · 1997 · 395 citations
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Centre National de la Recherche Scientifique
Paris, France
33 h-index
130 publications
14.4K citations

Chinese Academy of Sciences
Beijing, China
20 h-index
55 publications
4.6K citations
Universidade de São Paulo
São Paulo, Brazil
17 h-index
45 publications
2K citations

Monash University
Melbourne, Australia
16 h-index
46 publications
1.8K citations

University of Leeds
Leeds, United Kingdom
16 h-index
36 publications
1.9K citations

Université de Montpellier
Montpellier, France
15 h-index
24 publications
2.1K citations

Australian National University
Canberra, Australia
15 h-index
27 publications
1.9K citations

University of Oslo
Oslo, Norway
15 h-index
23 publications
945 citations
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JGR · 25 publications · 2.9K citations
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