3 edition of Geology of drill hole USW VH-2, and structure of Crater Flat, southwestern Nevada found in the catalog.
Geology of drill hole USW VH-2, and structure of Crater Flat, southwestern Nevada
Wilfred James Carr
Published
1985
by U.S. Dept. of the Interior, Geological Survey in Denver, Colo
.
Written in
Edition Notes
Statement | by W.J. Carr and L.D. Parrish ; prepared in cooperation with the Nevada Operations Office, U.S. Department of Energy (Interagency Agreement DE-A108-78ET44802) |
Series | Open-file report -- 85-475., Open-file report (Geological Survey (U.S.)) -- 85-475. |
Contributions | Parrish, L. D., United States. Dept. of Energy. Nevada Operations Office., Geological Survey (U.S.) |
The Physical Object | |
---|---|
Format | Microform |
Pagination | 1 v. |
ID Numbers | |
Open Library | OL17802979M |
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A meter ( ft) drill hole in Crater Flat shows the absence of buried Pliocene or Quaternary volcanic rocks, and penetrates a section of Timber Mountain, Paintbrush, and the upper part of and structure of Crater Flat Crater Flat Tuffs, similar to that exposed adjacent to Crater Flat.
A prominent negative aeromagnetic. Geology of drill hole USW VH-2, and structure of Crater Flat, southwestern Nevada (USGS-OFR) [Wilfred James Carr] on *FREE* shipping on qualifying : Wilfred James Carr. Get this from a library. Geology of drill hole USW VH-2, and structure of Crater Flat, southwestern Nevada.
[Wilfred James Carr; L D Parrish; United States. Department of Energy. Nevada Operations Office.; Geological Survey (U.S.)]. Geology of drill hole USW VH-2, and structure of Crater Flat, southwestern Nevada (USGS-OFR) by Wilfred James Carr | Jan 1, Unknown Binding.
Study of three trenches excavated across two faults along the eastern edge of Crate Flat indicates that the main fault movement offset unit QTa in trench 1 at least m down to the west, and occurred about m.y. ago, as indicated by included basalt ash. Later fault movement, detected in trench.
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management studies at the Nevada Test Site and the Waste Isolation Pilot Plant site, New Mexico, January 1,to Decemby V. Glanzman, 24 p., Free-air gradient observations in Yucca Flat, Nevada Test Site, by Philip S.
Powers and Don L. Healey, 18 p., Author: V.M. Glanzman. Open Library is an open, editable library catalog, building towards a web page for every book ever published. The Crater Flat-Prospector Pass caldera model was formulated by Carr (, ) to account for two major tectonic problems: the then unknown source for the Crater Flat Group, and the form and structure of Crater Flat basin.
Briefly, the model postulates that Crater Flat basin reflects the structure of a subsided (now buried. Download Citation | Hydraulic tests of Miocene volcanic rocks at Yucca Mountain and Pahute Mesa and implications for groundwater flow in the Southwest Nevada Volcanic Field, Nevada and California.
The geology of the area, like much of the Gr eat Basin of Nevada, is dominated by Basin and Range physiographic pr ovince character- ized by elongated, north-trending, fault-bounded mountain r anges. NDOT unnumbered map book County Maps, Nevada,by the Nevada Highway Department (now Nevada Department of Transportation), 49 oversized maps.
Nevada Division of Minerals unnumbered report for children Geothermal resources in Nevada,by S. Hodgson, D. Whiting, J. Spriggs, and L. Jacox, 27 p. The Yucca Mountain site is located in Nye County, approximately kilometers (90 miles) northwest of Las Vegas, Nevada, and on the southwestern boundary of the Nevada Test Site.
Yucca Mountain is an irregularly shaped elevated land mass six to 10 km wide (four. Altered phenotypic expression of immunoglobulin heavy-chain variable-region (VH) genes in Alicia rabbits probably reflects a small deletion in the VH genes closest to the joining.
Full text of "Nuclear waste program: hearings before the Committee on Energy and Natural Resources, United States Senate, One hundredth Congress, first other formats. Genetic diversity of the human immunoglobulin heavy chain VH region.
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