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Slipping interfaces: A possible source of S radiation from explosive sources

Salvado, Carlos and Minster, J. Bernard (1980) Slipping interfaces: A possible source of S radiation from explosive sources. Bulletin of the Seismological Society of America, 70 (3). pp. 659-670. ISSN 0037-1106. https://resolver.caltech.edu/CaltechAUTHORS:20140902-133653772

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Abstract

We consider the problem of reflection and refraction of purely compressional waves incident on an interface separating identical solid half-spaces in which the condition of continuity of shear displacement at the boundary is generalized to one that allows slippage. The problem is solved using the Cagniard-de Hoop technique. It is found that the generation of reflected P and S waves, as well as transmitted S waves, is most effective in the case of perfectly unbounded half-spaces. We discuss the implications of this model for the generation of S waves by block movement in the vicinity of an underground explosion.


Item Type:Article
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http://bssa.geoscienceworld.org/content/70/3/659.abstractPublisherArticle
Additional Information:© 1980 Seismological Society of America. Manuscript received September 4, 1979. The authors are grateful for many helpful critical comments and suggestions by members of the Seismological Laboratory and elsewhere, particularly those of C. B. Archambeau, L. Burdick, R. Butler, D. Harkrider, T. Heaton, D. Helmberger, G. Mellman, and J. Rudnicki. This research was conducted by the Advanced Research Project Agency of the Department of Defense and was monitored by the Air Force Office of Scientific Research under Contract AFOSR F49620-77-C-0022.
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Advanced Research Projects Agency (ARPA)UNSPECIFIED
Air Force Office of Scientific Research (AFOSR)F49620-77-C-0022
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Caltech Division of Geological and Planetary Sciences3148
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Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:49124
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:03 Sep 2014 23:52
Last Modified:03 Oct 2019 07:10

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