Strike-slip Deformation
Strike-Slip Deformation is a type of brittle geologic deformation characterized by predominantly horizontal displacement along a fault plane, where the relative motion of adjacent crustal blocks is parallel to the strike of the fault, distinguishing it from dip-slip and oblique-slip deformation mechanisms.
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Oblique Stepwise Rise and Growth of the Tibet Plateau
Paul Tapponnier, Xu Zhiqin, Françoise Roger et al. · Science · 2001 · 3.9K citations
Arthur G. Sylvester · Geological Society of America Bulletin · 1988 · 1.4K citations
Ronald E. Wilcox, T. P. Harding, D. R. Seely · AAPG Bulletin · 1973 · 1.1K citations
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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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299 publications
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Institut de physique du globe de Paris
Paris, France
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124 publications
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California Institute of Technology
Pasadena, United States
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111 publications
9K citations
University of Cambridge
Cambridge, United Kingdom
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University of Oxford
Oxford, United Kingdom
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Stanford University
Stanford, United States
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Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
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GJI · 211 publications · 16.3K citations
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BSSA · 249 publications · 14.9K citations
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JGS · 114 publications · 8.7K citations
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