The deuterium content of hydrous minerals from the East-Central Sierra Nevada and Yosemite National Park

Details The deuterium content of hydrous minerals from the East-Central Sierra Nevada and Yosemite National Park The deuterium content of hydrous minerals from the East-Central Sierra Nevada and Yosemite National Park

Dec 1962

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1962gecoa..26.1215g&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 26, Issue 12, pp.1215-1245

Physics

17

Scientific paper

The experimental procedure for the extraction of hydrogen from natural hydrous silicate minerals is outlined. 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. These data are discussed in relation to the petrogenesis of the principal rock types of the regions. Local hydrogen isotopic fractionation and equilibrium between coexisting hydrous silicates were noted.

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