Electrical resistivity structure at the SAFOD site from magnetotelluric exploration

Details Electrical resistivity structure at the SAFOD site from magnetotelluric exploration Electrical resistivity structure at the SAFOD site from magnetotelluric exploration

May 2004

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004georl..3112s05u&link_type=abstract

Geophysical Research Letters, Volume 31, Issue 12, CiteID L12S05

Physics

9

Seismology: Earthquake Dynamics And Mechanics, Seismology: Seismicity And Seismotectonics, Structural Geology: Fractures And Faults, Tectonophysics: Dynamics, Seismotectonics

Scientific paper

The magnetotelluric dataset collected on the San Andreas Fault at Parkfield has been re-analyzed using superior inversion algorithms that have been developed in recent years. A combination of constrained inversion, forward modeling and synthetic inversion studies are used, and show that at the SAFOD site, the low resistivity fault zone extends to a depth of 2-3 km. An extended zone of low resistivity east of the San Andreas Fault may be connected to the SAF at seismogenic depths. The connection increases along the SAF to the northwest and may be related to the transition from locked to creeping seismic behavior.

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