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Title: Preliminary assessment of the geothermal resource potential of the Yuma area, Arizona

Technical Report ·
DOI:https://doi.org/10.2172/6951323· OSTI ID:6951323

The Yuma area has had a long and complex tectonic history. The most southwesterly corner of the area presently comprises a small segment of the Salton Trough, a deep sediment-filled structural depression. Known geothermal anomalies in the Salton Trough make the Yuma area a favorable exploration target even though spreading-center heat sources are not expected to occur there. Geological and geophysical investigations reveal that the area is made up of low, rugged northwest-trending mountains separated by deep sediment-filled basins. Relief is a result of both erosional and structural activity. Northwest-trending en-echelon faults bound the range fronts and the basins, and have created several horst blocks (basement highs) that crop out at or near the surface. The Algodonnes fault is inferred to represent the northeast margin of the Salton Trough and apparently an inactive extension of the San Andreas fault system. Extensive well-pumping and applications of irrigation waters in recent years have created an unnatural state of flux in the hydrologic regime in the Yuma area. Gravity and aeromagnetic anomalies trend strongly northwest through the region as do lineaments derived from Landsat and Skylab photos. Electrical resistivity values in the Bouse Formation are exceptionally low, about 3 ohn-m. Heat flow appears to be normal for the Basin and Range province. Ground-water temperatures indicate zones of rising warm water, with one such warm anomaly confirmed by sparse geothermal-gradient data.

Research Organization:
Arizona Bureau of Geology and Mineral Technology, Tucson (USA). Geothermal Group
DOE Contract Number:
FC07-79ID12009
OSTI ID:
6951323
Report Number(s):
DOE/ID/12009-T3; ON: DE82021571
Resource Relation:
Other Information: Portions of document are illegible
Country of Publication:
United States
Language:
English