A Study of the Strong Ground Motion of the Borrego Mountain, California, Earthquake by Thomas


Several synthetic models are constructed to fit the first 40 sec of the transversely polarized displacement, as recorded at El Centro, of the April 9, 1968 Borrego Mountain earthquake. The modeling is done in the time domain using the response computed for a distributed set of point shear dislocations embedded in a layered half-space. The beginning 10 sec… (More)


7 Figures and Tables

Slides referencing similar topics