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• W2099578768 abstract "SUMMARY We develop a theory of seismic fracture utilizing the concepts of shear melting and the wetting transition. The basic mechanism involves the wetting of a pre-existing planar defect by a melted phase of microscopic width, eliminating friction forces on thin, almost planar regions. For fault regions of finite thickness this mechanism results in an order-of-magnitude increase in the creep rate, sufficient to initiate a macroscopic melt in the fault region. This model can explain observations of low-stress drops and small heat-flow anomalies in the neighbourhood of superficial faults, the cutoff in seismicity with depth in the San Andreas system, and the non-linear deformations observed near the fault trace." @default.
• W2099578768 created "2016-06-24" @default.
• W2099578768 creator A5080989902 @default.
• W2099578768 date "1988-07-01" @default.
• W2099578768 modified "2023-09-25" @default.
• W2099578768 title "Strain melting, the wetting transition and seismic instabilities" @default.
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• W2099578768 doi "https://doi.org/10.1111/j.1365-246x.1988.tb03432.x" @default.
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