Electrical structure in a region of the Transverse Ranges, southern California

Details Electrical structure in a region of the Transverse Ranges, southern California Electrical structure in a region of the Transverse Ranges, southern California

Mar 1977

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1977e%26psl..34..313r&link_type=abstract

Earth and Planetary Science Letters, vol. 34, no. 2, Mar. 1977, p. 313-320. Research supported by the California Institute of T

Computer Science

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Earthquakes, Electrical Resistivity, Magnetic Surveys, Southern California, Telluric Currents, Data Acquisition, Electrical Properties, Seismology, Two Dimensional Models

Scientific paper

Magnetotelluric sounding at a site in the Transverse Ranges province in southern California indicates a low-resistivity region in the lower crust and possibly also the upper mantle. A two-dimensional model fit to the data indicates that the resistivity of this region is between 1 and 10 ohm-meters. The depth to the top surface of this zone is between 15 and 20 km. The lateral extent of this feature, which strikes N65 deg W, appears to be confined to the Transverse Ranges province. The petrological characteristics of this region cannot be deduced unambiguously from the magnetotelluric sounding alone.

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