Arid
DOI10.2172/587919
报告编号USGS/WRIR--95-4132
来源IDOSTI_ID: 587919
Effect of faulting on ground-water movement in the Death Valley region, Nevada and California
Faunt, C.C.
英文摘要This study characterizes the hydrogeologic system of the Death Valley region, an area covering approximately 100,000 square kilometers. The study also characterizes the effects of faults on ground-water movement in the Death Valley region by synthesizing crustal stress, fracture mechanics,a nd structural geologic data. The geologic conditions are typical of the Basin and Range Province; a variety of sedimentary and igneous intrusive and extrusive rocks have been subjected to both compressional and extensional deformation. Faulting and associated fracturing is pervasive and greatly affects ground-water flow patterns. Faults may become preferred conduits or barriers to flow depending on whether they are in relative tension, compression, or shear and other factors such as the degree of dislocations of geologic units caused by faulting, the rock types involved, the fault zone materials, and the depth below the surface. The current crustal stress field was combined with fault orientations to predict potential effects of faults on the regional ground-water flow regime. Numerous examples of fault-controlled ground-water flow exist within the study area. Hydrologic data provided an independent method for checking some of the assumptions concerning preferential flow paths. 97 refs., 20 figs., 5 tabs.
出版年1997
报告类型Technical Report
语种英语
国家美国
来源学科分类58 GEOSCIENCES ; 05 NUCLEAR FUELS ; NEVADA TEST SITE ; HYDROLOGY ; YUCCA MOUNTAIN ; SITE CHARACTERIZATION ; RADIOACTIVE WASTE DISPOSAL ; GEOLOGY ; CALIFORNIA ; VALLEYS ; GEOLOGIC FAULTS ; GROUND WATER ; LIQUID FLOW ; CONTINENTAL CRUST ; STRESSES ; MAPS
URLhttp://www.osti.gov/scitech/servlets/purl/587919
资源类型科技报告
条目标识符http://119.78.100.177/qdio/handle/2XILL650/267387
推荐引用方式
GB/T 7714
Faunt, C.C.. Effect of faulting on ground-water movement in the Death Valley region, Nevada and California,1997.
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