Arid
DOI10.2172/6498569
报告编号USGS-PP-1044-H
来源IDOSTI_ID: 6498569
Reconnaissance of the hydrothermal resources of Utah
Rush, F.E.
英文摘要Geologic factors in the Basin and Range province in Utah are more favorable for the occurrence of geothermal resources than in other areas on the Colorado Plateaus or in the Middle Rocky Mountains. These geologic factors are principally crustal extension and crustal thinning during the last 17 million years. Basalts as young as 10,000 years have been mapped in the area. High-silica volcanic and intrusive rocks of Quaternary age can be used to locate hydrothermal convection systems. Drilling for hot, high-silica, buried rock bodies is most promising in the areas of recent volcanic activity. Southwestern Utah has more geothermal potential than other parts of the Basin and Range province in Utah. The Roosevelt Hot Springs area, the Cove Fort-Sulphurdale area, and the area to the north as far as 60 kilometers from them probably have the best potential for geothermal development for generation of electricity. Other areas with estimated reservoir temperatures greater than 150/sup 0/C are Thermo, Monroe, Red Hill (in the Monroe-Joseph Known Geothermal Resource Area), Joseph Hot Springs, and the Newcastle area. The rates of heat and water discharge are high at Crater, Meadow, and Hatton Hot Springs, but estimated reservoir temperatures there are less than 150/sup 0/C. Additional exploration is needed to define the potential in three additional areas in the Escalante Desert. 28 figs., 18 tabs.
出版年1983
报告类型Technical Report
语种英语
国家美国
来源学科分类15 GEOTHERMAL ENERGY ; UTAH ; GEOTHERMAL RESOURCES ; HOT SPRINGS ; HYDROLOGY ; KGRA ; RESOURCE ASSESSMENT ; FEDERAL REGION VIII ; NORTH AMERICA ; RESOURCES ; THERMAL SPRINGS ; USA ; WATER SPRINGS Geothermal Legacy
URLhttp://www.osti.gov/scitech/servlets/purl/6498569
资源类型科技报告
条目标识符http://119.78.100.177/qdio/handle/2XILL650/260095
推荐引用方式
GB/T 7714
Rush, F.E.. Reconnaissance of the hydrothermal resources of Utah,1983.
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