Thermal pressurization and onset of melting in fault zones

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Thermal pressurization and onset of melting in fault zones

[1] We examine how frictional heating drives the evolution of temperature, strength, and fracture energy during earthquake slip. For small slip distances, heat and pore fluid are unable to escape the shearing fault core, and the behavior is well approximated by simple analytical models that neglect any transport. Following large slip distances, the finite width of the shear zone is small compar...

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There are currently three major competing views on the nature of earthquake fault zones. The first is that faults are (possibly segmented and heterogeneous) Euclidean zones in a continuum solid. The second focuses on granular aspects of faults and deformation fields. The third is that faults are fundamentally rough fractal objects at all relevant scales. The existing data can not distinguish un...

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ژورنال

عنوان ژورنال: Journal of Geophysical Research

سال: 2006

ISSN: 0148-0227

DOI: 10.1029/2006jb004314