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Recognition of paleoearthquakes on the Puente Hills blind thrust fault, California
James F Dolan1, Shari A Christofferson, John H Shaw
1Department of Earth Sciences, University of Southern California, Los Angeles, CA 90089-0740, USA. dolan@earth.usc.edu
Abstract:
Borehole data from young sediments folded above the Puente Hills blind thrust fault beneath Los Angeles reveal that the folding extends to the surface as a discrete zone (=145 meters wide). Buried fold scarps within an upward- narrowing zone of deformation, which extends from the upward termination of the thrust ramp at 3 kilometers depth to the surface, document the occurrence of at least four large (moment-magnitude 7.2 to 7.5) earthquakes on this fault during the past 11,000 years. Future events of this type pose a seismic hazard to metropolitan Los Angeles. Moreover, the methods developed in this study can be used to refine seismic hazard assessments of blind thrusts in other metropolitan regions.
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