Thrust Faulting
Thrust faulting is a type of brittle deformation characterized by the low-angle reverse movement of rock masses along a fault plane, in which the hanging wall moves upward over the footwall due to compressional stresses, typically occurring within the context of continental collision, lithospheric deformation, mountain building, and Quaternary tectonics.
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Péter Molnár, Paul Tapponnier · Journal of Geophysical Research Atmospheres · 1978 · 781 citations
Jean‐Philippe Avouac, P. Tapponnier, Meixiang Bai et al. · Journal of Geophysical Research Atmospheres · 1993 · 777 citations · Full text
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Centre National de la Recherche Scientifique
Paris, France
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United States Geological Survey
Reston, United States
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Planetary Science Institute
Tucson, United States
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China Earthquake Administration
Beijing, China
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Massachusetts Institute of Technology
Cambridge, United States
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Institute of Geology, China Earthquake Administration
Beijing, China
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Institut de physique du globe de Paris
Paris, France
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Lamont-Doherty Earth Observatory
Sparkill, United States
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JGR · 58 publications · 7.7K citations
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GJI · 27 publications · 1.3K citations
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