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Determination of rupture duration and stress drop for earthquakes in southern California

Frankel, Arthur and Kanamori, Hiroo (1983) Determination of rupture duration and stress drop for earthquakes in southern California. Bulletin of the Seismological Society of America, 73 (6). pp. 1527-1551. ISSN 0037-1106. https://resolver.caltech.edu/CaltechAUTHORS:20140903-113319926

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Abstract

A simple technique is developed for determining the rupture duration and stress drop of earthquakes between magnitudes 3.5 and 4.0 using the time between the P-wave onset and the first zero crossing (τ_(1/2)) on seismograms from local seismic networks. This method is applied to 10 main shocks in southern California to investigate regional variations in stress drop. The initial pulse widths of 65 foreshocks or aftershocks of these events were measured. Values of τ_(1/2) for small earthquakes below about magnitude 2.2 are generally observed to remain constant with decreasing magnitude in four sequences studied. The relative pulse width of a particular main shock (M ≧ 3.5) at a given station is found to be correlated with the relative pulse width of its aftershocks recorded at that station. These observations are interpreted to signify that the waveforms of these small events (M ≦ 2.2) are essentially the impulse response of the path between the source and receiver. Values of τ_(1/2) determined from small foreshocks and aftershocks are, therefore, subtracted (in effect deconvolved) from those of each main shock to obtain an estimate of the rupture duration of the main shock which is corrected for path effects. Significant variations in rupture duration and stress drop are observed for the main shocks studied. Aftershock locations and azimuthal variations in τ_(1/2) both indicate that the rupture zone of one earthquake expanded unilaterally. A factor of 10 variation in stress drop is calculated for two adjacent events of similar seismic moments occurring 1 hr apart on the San Jacinto fault system. The first event in this pair had the highest stress drop of the events studied (860 bars) and was followed within 8 months by a magnitude 5.5 earthquake 2 km away.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://bssa.geoscienceworld.org/content/73/6A/1527.abstractPublisherArticle
ORCID:
AuthorORCID
Kanamori, Hiroo0000-0001-8219-9428
Additional Information:© 1983, by the Seismological Society of America. Manuscnpt received 6 May 1983. We thank Tom Heaton for reviewmg the manuscript. Jim Pechmann, Mary O'Ne1ll, Carl Johnson, Bill Bakun, and Bill Ellsworth provided useful discussions. Carl Johnson and Bernard Minster wrote the software to access the digital network data. We thank Bill Ellsworth and Jerry Eaton for their help in obtaining the analog tapes for the southern California network. The figures were drafted by Laszlo Lenches. This research was supported by the U.S. Geological Survey under Contract 14-08-0001-21210. One of the authors, (A. F.) was supported by a Bantrell Fellowship.
Funders:
Funding AgencyGrant Number
USGS14-08-0001-21210
Bantrell FellowshipUNSPECIFIED
Other Numbering System:
Other Numbering System NameOther Numbering System ID
Caltech Seismological Laboratory3880
Issue or Number:6
Record Number:CaltechAUTHORS:20140903-113319926
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20140903-113319926
Official Citation:Arthur Frankel and Hiroo Kanamori Determination of rupture duration and stress drop for earthquakes in southern California Bulletin of the Seismological Society of America, December 1983, v. 73, p. 1527-1551
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:49193
Collection:CaltechAUTHORS
Deposited By: Ruth Sustaita
Deposited On:03 Sep 2014 18:44
Last Modified:09 Mar 2020 13:18

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