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SHEAR HEATING IN CONTINENTAL STRIKE-SLIP SHEAR ZONES: MODEL AND FIELD EXAMPLES (1999)
A two-layer (crust and upper mantle), finite difference steady-state thermomechanical model of a long-lived (several million years) lithospheric strike-slip fault is presented, and its predictions compared with field observations from various major fault zones.
Reference:
Geophys. J. Int. (1999) 136, 19-40
Geophys. J. Int. (1999) 136, 19-40
Organization:
L aboratoire de tectonique et mecanique de la lithosphere
L aboratoire de tectonique et mecanique de la lithosphere
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