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Chapter Two - Rock friction

Published online by Cambridge University Press:  17 December 2018

Christopher H. Scholz
Christopher H. Scholz
Affiliation:
Lamont-Doherty Earth Observatory, Columbia University
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Summary

Once a fault has been formed its further motion is controlled by friction, which is a contact property rather than a bulk property. In the schizosphere the micromechanics of friction involve brittle fracture, but frictional behavior is fundamentally different from bulk brittle fracture. Here we examine this property in some detail and, in particular, discuss the stability of friction, which determines if fault motion is seismic or aseismic.

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The Mechanics of Earthquakes and Faulting , pp. 43 - 96
Publisher: Cambridge University Press
Print publication year: 2019

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