by Dept. of Energy, Division of Geothermal Energy, for sale by the National Technical Information Service] in [Washington], [Springfield, Va .
Written in English
|Statement||Jeffrey B. Hulen, Earth Science Laboratory, University of Utah Research Institute|
|Series||IDO ; 1701-1|
|Contributions||University of Utah. Research Institute. Earth Science Laboratory, United States. Dept. of Energy. Division of Geothermal Energy|
|The Physical Object|
|Pagination||iv, 31 p. :|
|Number of Pages||31|
Technical Report: Geology and alteration of the Coso Geothermal Area, Inyo County, California. Stanford Libraries' official online search tool for books, media, journals, databases, government documents and more. Alan E. Williams, "An Overview of the Geology and Geochemistry of the Coso Geothermal Area, Inyo County, CA.", The Diversity of Mineral and Energy Resources of Southern California, Michael A. . Report: Geology and alteration of the Coso Geothermal Area, Inyo County, California Abstract Geology and alteration of the Coso geothermal area were mapped in conjunction with geophysical surveys and a deep drill test (CGEH-1) to facilitate selection of a follow-up drill site.
Geological and geophysical analysis of Coso Geothermal Exploration Hole No. 1 (CGEH-1), Coso Hot Springs KGRA, California. The Coso area has ample surface evidence of geothermal energy including fumaroles, hot springs, hydrothermally altered rocks, and Late Cenozoic volcanics (as young as Pleistoc, YBP) including thirty-seven rhyolite domes. GEOLOGIC HISTORY OF THE COSO GEOTHERMAL SYSTEM Michael C. Adams, 1 Joseph N. Moore, 1 Steven Bjornstad, 2 and David I. Norman 3 1 Earth & Geoscience Institute, Wakara Way, SLC UT 2 Geothermal Program Office, G00D NAWS-CL, China Lake CA 3 New Mexico Tech, Socorro NM Keywords: Coso, fluid geochemistry, fluid inclusions, gase- ous species. Geology and alteration mapping analyzed exposed rocks in geothermal region. Neither geologic mapping nor deep drilling have revealed potential deep primary aquifers. Surface alteration at Coso is of three main types: (1) clay-opal-alunite alteration, (2) weak argillic alteration, and (3) stockwork calcite veins and veinlets, which are locally.
Get this from a library! Geology and alteration of the Coso geothermal area, Inyo County, California. [Jeffrey B Hulen; University of Utah. Research Institute. Earth Science Laboratory.; United States. Department of Energy. Division of Geothermal Energy.]. One well-cited example of an off-diagonal approach is the study by Newman et al. of the East Flank of the Coso geothermal system in eastern California. Newman et al. () imaged a subvertical low-resistivity (∼5 Ohm m) feature in a zone of major geothermal energy production, and interpreted it as a zone of high temperature fluids residing. The Coso Geothermal Exploration Hole number one (CGEH-1) was drilled in the Coso Hot Springs KGRA, California, from September 2 to December 2, Chip samples were collected at ten foot intervals and extensive geophysical logging surveys were conducted to . Geology and Geophysics. Exploration Geophysics; Geodesy and Gravity Heat flow in the Coso Geothermal Area, Inyo County, California. Jim Combs; Pages: ; First Published: 10 May ; Abstract; PDF; References; Hydrothermal alteration enthalpy and heat flow in the Roosevelt Hot Springs Thermal Area, Utah.