Geologic And Tectonic History Western Snake River Plain Wood And Clemens Pdf

geologic and tectonic history western snake river plain wood and clemens pdf

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Metrics details. A geothermal exploration corehole was drilled to a total depth of The corehole was used to collect an unusually large amount of data, including uniaxial compressive stress UCS experiments on core samples, to evaluate the geothermal potential of the western Snake River Plain.

Geologic and Tectonic History of the Western Snake River Plain, Idaho and Oregon

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Lamb, Lee M. Liberty, R. Blakely, T. Pratt, B. Sherrod, and Kasper van Wijk. Mikesell, Kasper van Wijk, Matthew M. Haney, John H.

Geologic and Tectonic History of the Western Snake River Plain, Idaho and Oregon

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The system can't perform the operation now. Try again later. Citations per year. Duplicate citations. The following articles are merged in Scholar.

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A geothermal exploration corehole was drilled to a total depth of The corehole was used to collect an unusually large amount of data, including uniaxial compressive stress UCS experiments on core samples, to evaluate the geothermal potential of the western Snake River Plain. In addition, unlike many exploration holes in this region, a fluid entry was encountered at A maximum temperature of

We present integrated geophysical data to characterize a geothermal system at Neal Hot Springs in eastern Oregon. This system is currently being developed for geothermal energy production. The hot springs are in a region of complex and intersecting fault trends associated with two major extensional events, the Oregon-Idaho Graben and the Western Snake River Plain. The intersection of these two fault systems, coupled with high geothermal gradients from thin continental crust produces pathways for surface water and deep geothermal water interactions at Neal Hot Springs. This basin-bounding fault serves as the primary conduit for deep water circulation.

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 Дэвид! - крикнула .

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