Abstract
Arrival-time data from 453 local earthquakes and 6 explosions at Parkfield,
CA, are inverted for earthquake locations and three-dimensional Vp
and Vp/Vs structure. The structure is dominated by the velocity contrast
across the SAF, with the southwest side about 20-25\% faster, consistent
with previous studies. Nearly all the earthquakes occur almost directly
beneath the fault trace. We find high-Vp/Vs anomalies that correlate
with low-resistivity features in a magnetotelluric model that are
interpreted to represent fluids. We locate a magnitude 2 earthquake
that is a potential target event for the final stage of SAFOD drilling,
yielding a depth of 3.1 km below surface and an epicenter 100 m southwest
of the fault trace. Nonlinear analyses indicate 95\%-confidence relative
and absolute uncertainties on the order of 500-700 m vertically and
200-300 m horizontally for this target earthquake.
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