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crushing and melting rock

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crushing and melting rock

of localised crushing and melting of the host rock during rapid (≥1.0 m/s) fault slip (McKenzie and Brune 1972; Sibson 1975; Cowan 1999). In the outcrop scale, pseudotachylyte usually occurs as a network of veins, filling the fractures associated with a fault zone. Texturally, pseudotachylyte is composed of numerous fragments (clasts) of the

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