Arid
DOI10.2172/5871587
报告编号USGS-OFR-82-111
来源IDOSTI_ID: 5871587
Gravity survey of Dixie Valley, west-central Nevada
Schaefer, D.H.
英文摘要Dixie Valley, a northeast-trending structural trough typical of valleys in the Basin and Range Province, is filled with a maximum of about 10,000 feet of alluvial and lacustrine deposits, as estimated from residual-gravity measurements obtained in this study. On the basis of gravity measurements at 300 stations on nine east-west profiles, the gravity residuals reach a maximum of 30 milliGals near the south-central part of the valley. Results from a three-dimensional inversion model indicate that the central depression of the valley is offset to the west of the geographic axis. This offset is probably due to major faulting along the west side of the valley adjacent to the Stillwater Range. Comparison of depths to bedrock obtained during this study and depths obtained from a previous seismic-refraction study indicates a reasonably good correlation. A heterogeneous distribution of densities within the valley-fill deposits would account for differing depths determined by the two methods. 17 refs., 4 figs., 2 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 ; GEOTHERMAL RESOURCES ; EXPLORATION ; NEVADA ; GRAVITY SURVEYS ; ALLUVIAL DEPOSITS ; GEOLOGIC STRUCTURES ; HOT SPRINGS ; FEDERAL REGION IX ; GEOLOGIC DEPOSITS ; GEOPHYSICAL SURVEYS ; NORTH AMERICA ; RESOURCES ; SURVEYS ; THERMAL SPRINGS ; USA ; WATER SPRINGS Geothermal Legacy
URLhttp://www.osti.gov/scitech/servlets/purl/5871587
资源类型科技报告
条目标识符http://119.78.100.177/qdio/handle/2XILL650/260091
推荐引用方式
GB/T 7714
Schaefer, D.H.. Gravity survey of Dixie Valley, west-central Nevada,1983.
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