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Page 12, results 276 - 300

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Lithium in the brines of Fish Lake Valley and Columbus Salt Marsh, Nevada
C. L. Smith, Allen L. Meier, H.D. Downey
1977, Open-File Report 77-54
Analyses of waters-from springs in Nevada have led to the identification of an area containing anomalous amounts of lithium northwest of the Clayton Valley-area. Fish Lake Valley and Columbus Salt Marsh contain waters having, relatively high lithium and potassium concentrations. At least a part of these waters is probably derived...
Genesis of a zoned granite stock, Seward Peninsula, Alaska
Travis Hudson
1977, Open-File Report 77-35
A composite epizonal stock of biotite granite has intruded a diverse assemblage of metamorphic rocks in the Serpentine Hot Springs area of north-central Seward Peninsula, Alaska. The metamorphic rocks include amphibolite-facies orthogneiss and paragneiss, greenschist-facies fine-grained siliceous and graphitic metasediments, and a variety of carbonate rocks. Lithologic units within the...
Epithermal beryllium deposits in water-laid tuff, western Utah
David A. Lindsey
1977, Economic Geology (72) 219-232
Epithermal beryllium deposits in western Utah have distinctive geological and geochemical associations that provide guides to exploration for new resources of beryllium and associated metals. Beryllium deposits at Spor Mountain and the Honeycomb Hills are uniquely associated with topaz-bearing rhyolite of Late Tertiary age and are restricted to porous water-laid...
Sterility among female lizards (Uta stansburiana) exposed to continuous gamma irradiation
F.B. Turner, P.A. Medica
1977, Radiation Research (70) 154-163
A natural population of the lizard Uta stansburiana occupying a fenced 9-ha area in southern Nevada was exposed to essentially continuous γ irradiation from an artificial source between February 1964 and September 1973. Tissue doses were estimated using implanted lithium fluoride microdosimeters. Females became sterile as early as 11 months...
Removal of fluorine and lithium from hectorite by solutions spanning a wide range of pH
Harry C. Starkey, Wayne Mountjoy, Johnnie M. Gardner
1977, Journal of Research of the U.S. Geological Survey (5) 235-242
One-gram samples of hectorite were treated with 40 millilitres each of hydrochloric acid (6 N), acetic acid (4.5 N), distilled water, natural seawater, sodium chloride (0.6 N), and sodium hydroxide (2.5 N) for 10 days in stoppered plastic centrifuge tubes. X-ray diffraction patterns show that the structure was virtually destroyed...
Radioactive mineral springs in Delta County, Colorado
Robert A. Cadigan, John N. Rosholt, J. Karen Felmlee
1976, Open-File Report 76-223
The system of springs in Delta County, Colo., contains geochemical clues to the nature and location of buried uranium-mineralized rock. The springs, which occur along the Gunnison River and a principal tributary between Delta and Paonia, are regarded as evidence of a still-functioning hydrothermal system. Associated with the springs are...
Lithium in sediments and rocks in Nevada
Robert G. Bohannon, Allen L. Meier
1976, Open-File Report 76-567
Reconnaissance geochemical sampling has been conducted by the Lithium Resource Program of the United States Geological Survey for much of the Western U.S. Sediment, rock, and brine samples have been collected in many states, but this report describes just those solid samples collected in Nevada. Further reports by other members...
Lithium in sediments and brines--how, why and where to search
James D. Vine
1975, Journal of Research of the U.S. Geological Survey (3) 479-485
The possibility of using lithium in batteries to power electric vehicles and as fuel for thermonuclear power has focused attention on the limited resources of lithium other than in pegmatite minerals. The Clayton Valley, Nev., subsurface lithium brine has been the major source of lithium carbonate since about 1967, but...
Rapid analysis of silicate, carbonate, and phosphate rocks: Revised edition
Leonard Shapiro
1975, Bulletin 1401
The rapid methods previously used by the U.S. Geological Survey to determine the major constituents of rocks have been modified to introduce atomic absorption spectrometry (AAS) where applicable. Two procedures are available for determining 10 constituents: one, from a single solution prepared by a nitric-acid dissolution of a lithium metaborate-lithium...
Movement of elements into the atmosphere from coniferous trees in subalpine forests of Colorado and Idaho
G.C. Curtin, H. D. King, E. L. Mosier
1974, Journal of Geochemical Exploration (3) 245-263
Exudates from conifer trees, presumably consisting largely of volatile materials, were sampled at 19 subalpine localitites in Colorado and Idaho where anomalous amounts of several metals were determined in vegetation and mull during previous geochemical testing. The trees sampled were lodgepole pine...
Lithium in surficial materials of the conterminous United States and partial data on cadmium
Hansford T. Shacklette, J.G. Boerngen, J.P. Cahill, R.L. Rahill
1973, Circular 673
Concentrations of lithium in 912 samples of soils and other regoliths from sites approximately 50 miles apart throughout the United States are represented on a map by symbols showing five ranges of values. A histogram of the lithium concentrations is also given. The geometric mean lithium concentration is 20.4 ppm...
Identification of a lithium-bearing smectite from Spor Mountain, Utah
Harry C. Starkey, Wayne Mountjoy
1973, Journal of Research of the U.S. Geological Survey (1) 415-419
Chemical analyses, X-ray diffraction data, and cation exchange determinations are given for a lithium-bearing smectite. The X-ray data and Greene-Kelly's lithium test indicate the presence of both dioctahedral and trioctahedral phases. The exchange determinations indicate that the lithium is in the structure of the clay, and the chemical data are intermediate between those for hectorite...