Transform Fault Motion
Transform Fault Motion is a type of plate boundary interaction characterized by the lateral, shear displacement of tectonic plates along strike-slip faults that offset segments of mid-ocean ridges or other plate margins, distinguishing it from divergent and convergent plate motions by the absence of crustal creation or destruction at the fault line.
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Charles DeMets, Richard G. Gordon, Donald F. Argus et al. · Geophysical Journal International · 1990 · 3.7K citations · Full text
J. B. Minster, T. H. Jordan · Journal of Geophysical Research Atmospheres · 1978 · 2.3K citations · Full text
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University of California, Santa Barbara, United States
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Centre National de la Recherche Scientifique
Paris, France
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97 publications
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Woods Hole Oceanographic Institution
Falmouth, United States
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United States Geological Survey
Reston, United States
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28 publications
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Scripps Institution of Oceanography
La Jolla, United States
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Institut de physique du globe de Paris
Paris, France
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University of California San Diego
San Diego, United States
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Sorbonne Université
Paris, France
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Lamont-Doherty Earth Observatory
Sparkill, United States
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JGR · 77 publications · 10.1K citations
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GJI · 22 publications · 4.7K citations
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