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FINE-SCALE STRUCTURE OF THE SAN ANDREAS FAULT ZONE AND LOCATION OF THE SAFOD TARGET EARTHQUAKES (2004)
In this paper are presented results from the tomographic analysis of seismic data from the Parkfield area using three different inversion codes. The models provide a consistent view of the complex velocity structure in the vicinity of the San Andreas, including a sharp velocity contrast across the fault.
Reference:
GEOPHYSICAL RESEARCH LETTERS, VOL. 31, 2004
GEOPHYSICAL RESEARCH LETTERS, VOL. 31, 2004
Organization:
Department of Geology and Geophysics, University of Wisconsin-Madison, Madison, Wisconsin, USA
USA, California
Department of Geology and Geophysics, University of Wisconsin-Madison, Madison, Wisconsin, USA
USA, California
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