Thermal regime in the Dixie Valley geothermal system

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Conference Paper: Thermal regime in the Dixie Valley geothermal system

Abstract
The thermal setting of the Dixie Valley geothermal systemis summarized. New data from shallow and deep wellsrequire that the geothermal system be a complex, steeplydipping fault zone with flow on a number of strands of thefault zone rather than a single fault plane. As a result of thisnew model for the reservoir in Dixie Valley there appear tobe numerous untested structures with evidence of fluid flow.The model has applications to other fault controlled, deepcirculation systems.

Authors 
David D. Blackwell, Bobbie Golan and Dick Benoit






Conference 
Proceedings World Geothermal Congress 2000; Tohoku, Japan; 2000


Published 
Proceedings World Geothermal Congress;, 2000





DOI 
Not Provided
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Online 
Internet link for Thermal regime in the Dixie Valley geothermal system

Citation

David D. Blackwell,Bobbie Golan,Dick Benoit. 2000. Thermal regime in the Dixie Valley geothermal system. In: Proceedings World Geothermal Congress. Proceedings World Geothermal Congress 2000; 2000; Tohoku, Japan. Tohoku, Japan: (!) ; p. 991-996