Abstract
Magnetotelluric and seismic reflection surveys at Parkfield, California,
show that the San Andreas fault zone is characterized by a vertical
zone of low electrical resistivity. This zone is 500 m wide and extends
to a depth of 4000 m. The low electrical resistivity is attributed
to high porosity of saline fluids present in the highly fractured
fault zone. The occurrence of microearthquakes and creep in the low
resistivity zone is consistent with suggestions that seismicity at
Parkfield is fluid driven.
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