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Silver Peak Innovative Exploration Project (Ram Power Inc.)

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Data generated from the Silver Peak Innovative Exploration Project, in Esmeralda County, Nevada, encompasses a deep-circulation (amagmatic) meteoric-geothermal system circulating beneath basin-fill sediments locally blanketed with travertine in western Clayton Valley (lithium-rich brines from which have been mined for several decades). Spring- and shallow-borehole thermal-water geochemistry and geothermometry suggest that a Silver Peak geothermal reservoir is very likely to attain the temperature range 260- 300oF (~125-150oC), and may reach 300-340oF (~150-170oC) or higher (GeothermEx, Inc., 2006). Results of detailed geologic mapping, structural analysis, and conceptual modeling of the prospect (1) support the GeothermEx (op. cit.) assertion that the Silver Peak prospect has good potential for geothermal-power production; and (2) provide a theoretical geologic framework for further exploration and development of the resource.

The Silver Peak prospect is situated in the transtensional (regional shearing coupled with extension) Walker Lane structural belt, and squarely within the late Miocene to Pliocene (11 Ma to ~5 Ma) Silver Peak-Lone Mountain metamorphic core complex (SPCC), a feature that accommodated initial displacement transfer between major right-lateral strike- slip fault zones on opposite sides of the Walker Lane. The SPCC consists essentially of a ductiley-deformed lower plate, or core, of Proterozoic metamorphic tectonites and tectonized Mesozoic granitoids separated by a regionally extensive, low-angle detachment fault from an upper plate of severely stretched and fractured structural slices of brittle, Proterozoic to Miocene-age lithologies. From a geothermal perspective, the detachment fault itself and some of the upper-plate structural sheets could function as important, if secondary, subhorizontal thermal-fluid aquifers in a Silver Peak hydrothermal system.

Citation Formats

Ram Power, Inc.. (2010). Silver Peak Innovative Exploration Project (Ram Power Inc.) [data set]. Retrieved from https://dx.doi.org/10.15121/1148794.
Export Citation to RIS
Miller, Clay. Silver Peak Innovative Exploration Project (Ram Power Inc.). United States: N.p., 01 Jan, 2010. Web. doi: 10.15121/1148794.
Miller, Clay. Silver Peak Innovative Exploration Project (Ram Power Inc.). United States. https://dx.doi.org/10.15121/1148794
Miller, Clay. 2010. "Silver Peak Innovative Exploration Project (Ram Power Inc.)". United States. https://dx.doi.org/10.15121/1148794. https://gdr.openei.org/submissions/268.
@div{oedi_3113, title = {Silver Peak Innovative Exploration Project (Ram Power Inc.)}, author = {Miller, Clay.}, abstractNote = {Data generated from the Silver Peak Innovative Exploration Project, in Esmeralda County, Nevada, encompasses a deep-circulation (amagmatic) meteoric-geothermal system circulating beneath basin-fill sediments locally blanketed with travertine in western Clayton Valley (lithium-rich brines from which have been mined for several decades). Spring- and shallow-borehole thermal-water geochemistry and geothermometry suggest that a Silver Peak geothermal reservoir is very likely to attain the temperature range 260- 300oF (~125-150oC), and may reach 300-340oF (~150-170oC) or higher (GeothermEx, Inc., 2006). Results of detailed geologic mapping, structural analysis, and conceptual modeling of the prospect (1) support the GeothermEx (op. cit.) assertion that the Silver Peak prospect has good potential for geothermal-power production; and (2) provide a theoretical geologic framework for further exploration and development of the resource.

The Silver Peak prospect is situated in the transtensional (regional shearing coupled with extension) Walker Lane structural belt, and squarely within the late Miocene to Pliocene (11 Ma to ~5 Ma) Silver Peak-Lone Mountain metamorphic core complex (SPCC), a feature that accommodated initial displacement transfer between major right-lateral strike- slip fault zones on opposite sides of the Walker Lane. The SPCC consists essentially of a ductiley-deformed lower plate, or core, of Proterozoic metamorphic tectonites and tectonized Mesozoic granitoids separated by a regionally extensive, low-angle detachment fault from an upper plate of severely stretched and fractured structural slices of brittle, Proterozoic to Miocene-age lithologies. From a geothermal perspective, the detachment fault itself and some of the upper-plate structural sheets could function as important, if secondary, subhorizontal thermal-fluid aquifers in a Silver Peak hydrothermal system.}, doi = {10.15121/1148794}, url = {https://gdr.openei.org/submissions/268}, journal = {}, number = , volume = , place = {United States}, year = {2010}, month = {01}}
https://dx.doi.org/10.15121/1148794

Details

Data from Jan 1, 2010

Last updated Aug 19, 2021

Submitted Nov 20, 2013

Organization

Ram Power, Inc.

Contact

Clay Miller

775.398.3720

Authors

Clay Miller

Ram Power Inc.

Research Areas

DOE Project Details

Project Name Recovery Act: Silver Peak Innovative Exploration Project

Project Lead Mike Weathers

Project Number EE0002844

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