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EARTHQUAKE FOCAL MECHANISMS IN THE EASTERN TRANSVERSE RANGES AND SAN EMIGDIO MOUNTAINS, SOUTHERN CALIFORNIA AND EVIDENCE FOR A REGIONAL DECOLLEMENT
(1985)
Abstract
Earthquake focal mechanisms obtained from P-wave first motions are pre- sented for the Eastern Transverse Ranges and the San Emigdio Mountains in Southern California. The former region shows a predominance of strike-slip faulting whereas Quaternary faults in the region show thrust motion. We suggest that the observed strike-slip mode of d...More
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