Thrust Fault Systems
Thrust Fault Systems is a structural geological construct that characterizes networks of low-angle reverse faults in which crustal shortening is accommodated by the transport of upper-plate rock units over lower-plate units, typically in convergent tectonic settings associated with collision tectonics, planetary crustal deformation, and compressional orogenic systems.
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The seismogenic zone of subduction thrust faults
R. D. Hyndman, Makoto Yamano, D. A. Oleskevich · Island Arc · 1997 · 627 citations
Thomas Ader, Jean‐Philippe Avouac, Jing Liu‐Zeng et al. · Journal of Geophysical Research Atmospheres · 2012 · 595 citations
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United States Geological Survey
Reston, United States
23 h-index
119 publications
4.7K citations

Centre National de la Recherche Scientifique
Paris, France
21 h-index
83 publications
5.6K citations
California Institute of Technology
Pasadena, United States
14 h-index
38 publications
6.8K citations
China Earthquake Administration
Beijing, China
13 h-index
63 publications
4.6K citations
The University of Tokyo
Tokyo, Japan
12 h-index
21 publications
1.4K citations

Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
10 h-index
59 publications
3.3K citations
Geological Survey of Canada
Ottawa, Canada
9 h-index
11 publications
2K citations
University of California, Los Angeles
Los Angeles, United States
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15 publications
565 citations
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JGR · 36 publications · 3K citations
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