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Hydrogen isotope composition of deep-seated water

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Abstract

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. The mantle water seems to have aδD value of —85±10‰ on the basis of results of inclusions in the nodule-olivine.

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Authors and Affiliations

  1. Department of Geology, Shinshu University, Matsumoto, 390, Nagano Pref., Japan

    Yoshimasu Kuroda

  2. Marine Department, Japan Meteorological Agency, Õtemachi, 100, Tokyo, Japan

    Tetsuro Suzuoki

  3. Department of Chemistry, Tokyo Institute of Technology, O-okayam, Meguro-ku, 152, Tokyo, Japan

    Sadao Matsuo

Authors
  1. Yoshimasu Kuroda
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  2. Tetsuro Suzuoki
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  3. Sadao Matsuo
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Kuroda, Y., Suzuoki, T. & Matsuo, S. Hydrogen isotope composition of deep-seated water. Contr. Mineral. and Petrol. 60, 311–315 (1977). https://doi.org/10.1007/BF01166803

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  • DOI: https://doi.org/10.1007/BF01166803

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