Shear-wave anisotropy and the stress field from borehole recordings at 2.5 km depth at Cajon Pass
Author:
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/article-pdf/129/2/439/1598756/129-2-439.pdf
Reference33 articles.
1. Microseismicity on a locked section of the San Andreas Fault, recorded at 2.5 km depth in the Cajon Pass borehole;Abercrombie;J. geophys. Res.,1995
2. Near surface attenuation and site effects from comparison of surface and deep borehole recordings;Abercrombie;Bull. seism. Soc. Am.,1997
3. Source parameters of small earthquakes recorded at 2.5 km depth, Cajon Pass, Southern California; implications for earthquake scaling;Abercrombie;Geophys. Res. Lett.,1993
4. Suggestions for a consistent terminology for seismic anisotropy;Crampin;Geophys. Prospect.,1989
5. Effects of point singularities on shear-wave propagation in sedimentary basins;Crampin;Geophys. J. Int.,1991
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