A method for determination of the lower crustal structure along the San Andreas fault system in central California
1977 ◽
Vol 67
(3)
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pp. 793-807
Keyword(s):
abstract A method for determining lower crustal structure by comparing residuals of distant events, thereby reducing the effect of near-surface structure on seismic waves, has been tested through a straightforward numerical analysis of teleseismic residuals in central California. The results show a general crustal thinning to the west, with a sharp gradient along the San Andreas fault and a uniform crustal thickness between the San Andreas fault and the Calaveras and Hayward faults.
Keyword(s):
2001 ◽
Vol 113
(12)
◽
pp. 1580-1592
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Keyword(s):