Seismological Research Letters; July/August 2006; v. 77; no. 4;
p. 440-444; DOI: 10.1785/gssrl.77.4.440
© 2006 Seismological Society of America
The COMPLOC Earthquake Location Package
Guoqing Lin and
Peter Shearer
Scripps Institution of Oceanography, University
of California San Diego
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INTRODUCTION
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This article describes the programs included in the COMPLOC computer
program package that are designed to apply the source-specific station term
(SSST) method to solve for local earthquake locations using P- and
S-wave phase data. These programs can greatly improve the relative
location accuracy of nearby events by applying empirical corrections for the
biasing effects of three-dimensional velocity structure. They have been tested
on data from both the Southern California Seismic Network (SCSN) and Northern
California Seismic Network (NCSN)
The SSST method (Richards-Dinger and
Shearer 2000; Lin and Shearer
2005) works by assigning each station a travel-time correction
that varies as a function of source position. This approach provides relative
location accuracy comparable to master event or hypocentroidal decomposition
(Jordan and Sverdrup 1981)
methods within compact event clusters, but is applicable to distributed
seismicity. It has some similarities to the double-difference algorithm
(Waldhauser and Ellsworth 2000,
2002) and can be shown to give
comparable results in tests on synthetic data
(Lin and Shearer 2005).
However, the SSST approach has computational advantages for big data sets
because the location and station term parts of the computation are separate,
so that large matrix inversions are not necessary. In addition, our
implementation of SSST provides the option to use L1-norm misfit measures,
which are more robust than least squares in the case of occasional timing
errors or bad phase picks.
We implement the SSST approach by selecting nearby events located within a
sphere of specified radius rmax around the target event.
The station term for the target event is then computed as the median (or mean)
residual of these events. Different results will be obtained depending upon
the size of the cutoff distance rmax. If
rmax is set to a large enough . . . [Full Text of this Article]
Institute of Geophysics and Planetary Physics
Scripps
Institution of Oceanography
University of California San Diego
La Jolla,
CA 92093-0225
U.S.A.
gulin@ucsd.edu
pshearer@ucsd.edu
(G.L.,
P.S.)
Copyright © 2009 by Seismological Society of America