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Published December 1987 | Published
Journal Article Open

Epicentral confidence regions of nuclear test events at teleseismic distances

Abstract

The accurate location of seismic events is a basic discriminant for underground nuclear test monitoring (Bolt, 1976; Dahlman and Israelson, 1977; Blandford, 1982). Of particular interest are determining epicentral confidence regions and providing constraints on estimated focal depths. In this study, only routine teleseismic P travel-time data are used, as provided by worldwide stations reporting to the International Seismological Centre (ISC). This lessens the need to model the effects of crustal and shallow-mantle velocity variations, as is necessary with seismographic networks operating at regional distances (Blandford, 1981; Evernden et al., 1986).

Additional Information

© 1987 Seismological Society of America. Manuscript received 8 January 1987. Special thanks are in order to Dr. Timothy H. Dixon of the Jet Propulsion Laboratory for providing an opportunity to finish and present these results. This research was supported by Grant EAR-84167902 of the National Science Foundation and by the Director, Office of Basic Energy Sciences, Division of Engineering, Mathematics, and Geosciences, of the U.S. Department of Energy under Contract DE-AC03- 76SF00098. All computations were carried out at the Center for Computational Seismology of the Lawrence Berkeley Laboratory.

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