Continental Transform Faults is a geologic fault that serves as a tectonic boundary where two continental plates slide horizontally past each other within the Earth's lithosphere, distinguished by strike-slip motion and the absence of active volcanism typical of divergent or convergent boundaries.
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Charles DeMets, Richard G. Gordon, Donald F. Argus et al. · Geophysical Journal International · 1990 · 3.7K citations · Full text
Geodynamics: Applications of Continuum Physics to Geological Problems
Philip England · Eos · 1983 · 1.6K citations
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