期刊
GEOPHYSICAL RESEARCH LETTERS
卷 28, 期 6, 页码 1103-1106出版社
AMER GEOPHYSICAL UNION
DOI: 10.1029/2000GL012060
关键词
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Existing constitutive laws of rock friction cannot describe both observed strengthening in the absence of slip and frictional behavior around steady-state sliding. Combining existing rate- and state-dependent friction laws, we propose a new friction law which expresses logarithmically time-dependent healing at sliding velocities smaller than a cut-off velocity V-c and approaches the so-called slip law at velocities larger than V-c. Numerical simulations show that the new friction law adequately explains experimental results of velocity stepping tests and slidehold-slide tests, which have widely been used to examine velocity-, time-, and displacement-dependent property of rock friction. Because the new friction law has a simple form and appears appropriate for a wide range of conditions, it is useful for application to numerical modeling of seismic cycles.
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