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Published July 2002 | public
Journal Article

A Full Waveform Test of the Southern California Velocity Model by the Reciprocity Method

Abstract

We apply the reciprocity method (EISNER and CLAYTON, 2001a) to compare the full waveform synthetic seismograms with a large number of observed seismograms. The reciprocity method used in the finite-difference modeling allows for the use of high quality data observed from the earthquakes distributed over the wide range of azimuths and depths. We have developed a methodology to facilitate the comparison between data and synthetics using a set of attributes to characterize the seismograms. These attributes are maximum amplitude, time delay and coda decay of the magnitude of the displacement vector. For the Southern California Velocity Model, Version 1 (MAGISTRALE et al., 1996), we have found misfits between data and synthetics for paths traveling outside of the sedimentary basins and the western part of the Los Angeles and San Fernando basins.

Additional Information

© 2002 Birkhäuser Verlag, Basel. Received March 3, 2001, revised February 5, 2001, accepted August 28, 2001. The authors would like to thank the reviewer Harold Magistrale and the two anonymous reviewers for their valuable suggestions. Special thanks go to Jascha Polet and Dr. Donald Helmberger for their input. Many of the figures were made with GMT (WESSEL and SMITH, 1991). This research was supported by the Southern California Earthquake Center. SCEC is funded by NSF Cooperative Agreement EAR-8920136 and USGS Cooperative Agreements 14-08-0001-A0899 and 1434-HQ-97AG01718. The SCEC contribution number for this paper is 525.

Additional details

Created:
August 19, 2023
Modified:
October 19, 2023