Arid
报告编号DE20111022764
Role of Low-Angle Extensional Tectonics, Flat Fracture Domains, and Gravity Slides in Hydrothermal and EGS Resources of the Western United States.
Moore, J.
英文摘要The Steamboat Springs geothermal system provides the most dramatic example of subhorizontal thermal-fluid aquifers in crystalline rock in the Basin and Range, but this is by no means an isolated case. Similar but more diffuse subhorizontal permeability has been reported at Roosevelt Hot Springs and Cove-Fort Sulphurdale, Utah; and a km-scale gravity-slide block channels injectate at Dixie Valley, Nevada. During the course of this phase of the project 2543 reports including text, figures and large format enclosures, 1428 maps, and 698 well logs were scanned. The information is stored in a Microsoft Access Database on the Geothermal Server. Detailed geologic cross sections of the Desert Peak geothermal field were developed to identify the structural controls on the geothermal system and locate possible fluid flow paths. The results of this work were published by Lutz and others (2009, Appendix 1) in the Stanford Reservoir Engineering Conference Proceedings.
英文关键词Geothermal systems Reservoir engineering Geothermal fields Aquifers Cross sections Deserts Fluid flow Igneous rocks Metamorphic rocks Permeability Utah Tectonics Nevada Roosevelt hot springs Steamboat springs
出版年2011
语种英语
国家United States
URLhttp://r.cnki.net/KCMS/detail/detail.aspx?DbCode=KJBG&dbname=KJBGW&filename=59fb132a31c97d1d549ea8f6
来源机构Technical Information Center Oak Ridge Tennessee
资源类型科技报告
条目标识符http://119.78.100.177/qdio/handle/2XILL650/273761
推荐引用方式
GB/T 7714
Moore, J.. Role of Low-Angle Extensional Tectonics, Flat Fracture Domains, and Gravity Slides in Hydrothermal and EGS Resources of the Western United States.,2011.
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