Hydrogen extractions from silicate minerals by sodium carbonate fusion and its application to deuterium analyses of fluid inclusions in some olivines
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In this article, the authors measured the bulk hydrogen content and D/H ratio of the inclusion in olivine and showed that a consistent value of δD was obtained with a standard deviation of ± 2Abstract:
Fluid inclusions in olivine were extracted in vacuum by a sodium carbonate fusion method. In the present study, bulk hydrogen content and D/H ratio of the inclusion were measured. The results showed that a consistent value of δD was obtained with a standard deviation of ±2‰, when the absolute amount of hydrogen extracted was more than 40μmol (0.9ml STP H2). On the other hand, when the absolute amount of extracted hydrogen was less than 40μmol, δD value of the extract fluctuated, probably being affected by the contamination in the whole procedure.read more
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Hydrogen isotope composition of deep-seated water
TL;DR: In this paper, the D/H ratios of phlogopites and amphiboles from rocks of possible mantle origin and also those of water from (glass?) inclusions in olivines of the olivine nodule and peridotites have been determined.
References
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Conversion of Hydrogenic Materials to Hydrogen for Isotopic Analysis
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The deuterium content of hydrous minerals from the East-Central Sierra Nevada and Yosemite National Park☆
TL;DR: The experimental procedure for the extraction of hydrogen from natural hydrous silicate minerals is outlined in this paper, where the D/H ratios, water, and flourine contents have been determined for coexisting biotite, hornblende, and chlorite from rocks of the east-central Sierra Nevada and Yosemite National Park regions.
Journal ArticleDOI
The deuterium content of water in some volcanic glasses
Irving Friedman,Robert L. Smith +1 more
TL;DR: The deuterium-hydrogen composition (relative to Lake Michigan water = 0.0) of water extractsd from coexisting perlite and obsidian from eleven different localities was determined as discussed by the authors.
Journal ArticleDOI
The carbon, hydrogen, and oxygen isotopic composition of the hydrothermal fluids responsible for the lead-zinc deposits at Providencia, Zacatecas, Mexico
TL;DR: In this paper, the relative deuterium concentration of water in primary fluid inclusions in calcite, quartz, and sphalerite from several mines at Providencia, Zacatecas, Mexico, was determined to fall in the narrow range 6.8 to 8.3%.
Journal ArticleDOI
The Bluebell Mine, British Columbia; I, Mineralogy, paragenesis, fluid inclusions, and the isotopes of hydrogen, oxygen, and carbon
Hiroshi Ohmoto,Robert O. Rye +1 more
TL;DR: In this article, pressure, temperature, and depth of sulfide mineralization, geochemistry and origin of hydrothermal solutions, earlier fluids possibly juvenile, later fluids meteoric.
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