A transform fault is a
fault that is a special case of
strike-slip faulting which terminates abruptly, at both ends, at a major transverse geological feature. Also known as a conservative plate boundary.Transform faults comprise one of the three types of plate boundaries in
plate tectonics. This term was proposed by
J. Tuzo Wilson in 1965 and he particularly recognized the concept in the case of the transverse strike-slip faults along which
mid-oceanic ridges are off-set.
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