|Eastern Mojave Vegetation||Beowawe-Geyser Road, Eureka County, Nevada|
Topics in this Article:
|From Nevada State Route 306 south of Beowawe to The Geysers|
Other articles: Nevada State Route 306 at Beowawe-Geyser Rd
Junction: Nevada State Route 306
Locations: The Geysers.
The GeysersBanerjee, et al. (2011) assessed the relative importance of deeply circulating meteoric water and direct mantle fluid inputs on near-surface 3He/4He anomalies reported at the Coso and Beowawe geothermal fields of the western United States. The depth of meteoric fluid circulation is a critical factor that controls the temperature, extent of fluid-rock isotope exchange, and mixing with deeply sourced fluids containing mantle volatiles. The influence of mantle fluid flux on the reported helium anomalies appears to be negligible in both systems. This study illustrates the importance of deeply penetrating permeable fault zones (10-12 to 10-15 m2) in focusing groundwater and mantle volatiles with high 3He/4He ratios to shallow crustal levels. These continental geothermal systems are driven by free convection, and fluid flow is guided by faults rather than topographic gradients.
Literature CitedA list of all literature cited by this web site can be found in the Bibliography.
Banerjee, Amlan, Mark Person, Albert Hofstra, Donald Sweetkind, Denis Cohen, Andrew Sabin, Jeff Unruh, George Zyvoloski, Carl W. Gable, Laura Crossey, and Karl Karlstrom. 2011.
Deep permeable fault–controlled helium transport and limited mantle flux in two extensional geothermal systems in the Great Basin, United States.
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Date and time this article was prepared: 8/11/2018 2:22:51 PM