Changes in source and site effects compared to codaQ ?1 temporal variations using microearthquakes doublets in California-Reference-Cited by-同舟云学术

Changes in source and site effects compared to codaQ ?1 temporal variations using microearthquakes doublets in California

Published:1990-09 Issue:2 Volume:134 Page:195-228
ISSN:0033-4553
Container-title:Pure and Applied Geophysics PAGEOPH
language:en
Short-container-title:PAGEOPH

Author:

Got J. L.,Poupinet G.,Fr�chet J.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/BF00876998.pdf

Reference30 articles.

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2. Aki, K. (1985),Theory of Earthquake Prediction with Special References to Monitoring of the Quality Factor of Lithosphere by Coda Method, Earthq. Pred. Res.3, 219?230.

3. Bakun, W. H., Stewart, R. M., andBufe, C. G. (1978),Directivity in the High Frequency Radiation of Small Earthquakes, Bull. Seismol. Soc. Am.68, 1253?1263.

4. Chouet, B. (1979),Temporal Variation in the Attenuation of Earthquake Coda near Stone Canyon, California, Geophys. Res. Lett.6, 143?146.

5. Clymer, R. W., andMcEvilly, T. V. (1981),Travel-time Monitoring with Vibroseis *, Bull. Seismol. Soc. Am.71, 1903?1927.

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