Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.2172/5871587 |
报告编号 | USGS-OFR-82-111 |
来源ID | OSTI_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 |
URL | http://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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