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Numerical simulation of seismic cycles with a composite rate- and state-dependent friction law

Naoyuki Kato and Terry E. Tullis
Numerical simulation of seismic cycles with a composite rate- and state-dependent friction law
Bulletin of the Seismological Society of America (April 2003) 93 (2): 841-853

Abstract

Properties of rate- and state-dependent friction laws are examined through numerical simulations. Among several versions of the rate- and state-dependent friction laws, we use the slowness law, the slip law, and the composite law. The last was recently proposed by Kato and Tullis (2001) for better explaining experimental observations of rock friction in the laboratory. Two kinds of simulations are done. One is for cyclic stick-slip motion of a single degree of freedom spring-block system. The other is for seismic cycles at a subduction zone, where a 2D model of uniform elastic half-space is used. Assuming the same values of friction parameters, we compare the simulation results for the three friction laws. From the two kinds of simulations, we find that the recurrence interval of simulated earthquakes is the longest, and the magnitude of preseismic sliding is the smallest, for the composite law.


ISSN: 0037-1106
EISSN: 1943-3573
Coden: BSSAAP
Serial Title: Bulletin of the Seismological Society of America
Serial Volume: 93
Serial Issue: 2
Title: Numerical simulation of seismic cycles with a composite rate- and state-dependent friction law
Affiliation: Geological Survey of Japan/AIST, Institute of Geoscience, Tsukuba, Japan
Pages: 841-853
Published: 200304
Text Language: English
Publisher: Seismological Society of America, Berkeley, CA, United States
References: 44
Accession Number: 2003-049513
Categories: Seismology
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. 1 table
N36°27'00" - N36°27'00", E140°34'00" - E140°34'00"
Secondary Affiliation: Brown University, USA, United States
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2018, American Geosciences Institute.
Update Code: 200316

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