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U.S. Department of Energy
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Electrical resistivity survey of the Salton Sea geothermal field Imperial Valley, Calfornia. [Schlumberger, equatorial, and dipole-dipole soundings]

Technical Report ·
OSTI ID:7143455
An extensive electrical resistivity survey was conducted in the Salton Sea Geothermal Field, Imperial Valley, California. Very high energizing power (upward of 200 amperes) was employed to determine the extremely low resistivities (less than 0.5 ohmmeters) which were expected, to depths of 3 to 6 km. A combination of Schlumberger, equatorial, and dipole-dipole sounding techniques was employed and ultra-low commutation periods were used to avoid skin depth effects. Some depth soundings were extended into the sea by means of the equatorial sounding approach. The findings of the resistivity survey are combined with a previously reported marine seismic survey of the Salton Sea. They indicate that a very complex structural-hydrogeological pattern exists in the area. Integration of all existing data suggests that the Salton Sea geothermal field is an expression of active crustal spreading presently taking place along the southern shore of the Sea. The resistivity survey revealed the existence of six significant faults in the area. These are named here as the Wister, Calipatria, Red Hill, Brawley, Fondo and Westmorland Faults. The discovered faults act as either aquicludes or aquitards, probably with varying degrees of sealing effectiveness along their length. Comparison of existing isothermal maps, structural maps and the iso-resistivity data leads to the conclusion that sharp salinity gradients must exist in the area. Radical changes in vertical and lateral resistivity distributions suggest that a complex stratigraphic-temperature-salinity pattern exists in the area.
Research Organization:
California Univ., Livermore (USA). Lawrence Livermore Lab.
DOE Contract Number:
W-7405-ENG-48
OSTI ID:
7143455
Report Number(s):
UCRL-13690(Vols.1-2)
Country of Publication:
United States
Language:
English