Deuterium/Hydrogen Ratios and Water Content of Some Silicate Melts at High Pressure

  • Y. Hariya
  • Y. Kuroda
  • S. Matsuo
  • T. Suzuoki

Abstract

Various approaches have been made by different workers to determine the role of water in the mantle or the lower crust. For example, Kuroda et al. [1] determined the water content of some hydrosilicate minerals under high pressure and high temperature conditions. The stability field of some hydro-silicate minerals was studied by Kushiro [2], Kushiro et al. [3], Lambert and Wyllie [4], Hariya et al. [5,6] and others. The investigations of the role of water on the magma genesis (Allen et al. [7], Kushiro [8], and Burnham and Davis [9]) and the hydrogen and oxygen isotope frac-tionation of hydrous minerals (Kokubo et al. [10], Sheppard and Epstein [11], and Kuroda et al. [12]) also provide valuable information as to the concentration of water in the upper mantle or the lower crust.

Keywords

Quartz Depression Silicate Sodium Chloride Petrol 

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Copyright information

© Springer Science+Business Media New York 1979

Authors and Affiliations

  • Y. Hariya
    • 1
  • Y. Kuroda
    • 2
  • S. Matsuo
    • 3
  • T. Suzuoki
    • 4
  1. 1.Hokkaido UniversitySapporoJapan
  2. 2.Shinshu UniversityMatsumoto, NaganoJapan
  3. 3.Tokyo Institute of TechnologyTokyoJapan
  4. 4.Japan Meteorological AgencyTokyoJapan

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