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THERMAL PRESSURIZATION OF PORE FLUID DURING EARTHQUAKE SLIP (2009)

This thesis is intended as a detailed analysis of a candidate dynamic fault weakening mechanism called thermal pressurization of porefluid, based on the theory of thermoporoelasticity and on the latest geological, laboratory, and theoretical field results.

Reference:
Organization:
Comenius University, Faculty of Mathematics, Physics and Informatics, Department of Astronomy, Physics of the Earth, and Meteorology
Slovakia
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