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Isotopic Analysis At Geysers Area (Lambert & Epstein, 1992)
ExplorationOutcome useful  +
ExplorationTechnique Isotopic Analysis- Rock +
Notes Measurements of 180/160, 13C/12C and D/H r
Measurements of 180/160, 13C/12C and D/H ratio variations were made by the usual methods (McCrea, 1950; Taylor and Epstein, 1962; Epstein and Taylor, 1970) using mass spectrometers of the type described by Nier (1947) with modifications by McKinney et al. (1950). Results are reported in 8-notation with respect to the SMOW (Craig, 1961 ) and PDB (Urey et al., 1951 ) standards. Analytical precisions for multiple analyses of any single sample were _+ 0.2%0 for oxygen and carbon and _ 1%o for hydrogen. Inhomogeneities of cuttings fractions gave rise to variations within single cuttings fractions as large as _ 0.5%0 for oxygen and carbon and + 5%0 for hydrogen.
oxygen and carbon and + 5%0 for hydrogen.  +
OpenEI/PageDescription Isotopic Analysis At Geysers Area (Lambert & Epstein, 1992): geothermal exploration activity.  +
OpenEI/PageKeyword Geothermal  + , Geysers Area  + , Isotopic Analysis- Rock  +
Place Geysers Area +
Reference material Stable-Isotope Studies Of Rocks And Secondary Minerals In A Vapor-Dominated Hydrothermal System At The Geysers, Sonoma County, California +
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Isotopic Analysis At Geysers Area (Lambert & Epstein, 1992) + , Isotopic Analysis At Geysers Area (Lambert & Epstein, 1992) +
Categories Exploration Activities , Geothermal
Modification date
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17:13:27, 7 October 2013  +
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