Abstract
Chemistry dependence of δD of chlorites is inferred from data for natural chlorites. δD of water equilibrated with those chlorites is estimated to be −2∼−8‰.
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Kuroda, Y., Suzuoki, T., Matsuo, S., Kanisawa, S.: D/H fractionation of coexisting biotite and hornblende in some granitic rock masses. J. Japan. Assoc. Min. Pet. Econ. Geol. 69, 95–102 (1974)
Kuroda, Y., Suzuoki, T., Matsuo, S., Kanisawa, S.: D/H fractionation of coexisting biotite and hornblence in some granitic masses — A supplement. J. Japan. Assoc. Min. Pet. Econ. Geol. 70, 352–362 (1975a)
Kuroda, Y., Kinugawa, T., Suzuoki, T., Matsuo, S.: Origin of hornblendites in the Ōeyama (Kōmori) ultramafic body in view of hydrogen isotope study. Geoch. J. 9, 173–176 (1975b)
Shirozu, H.: X-ray powder patterns and cell dimensions of some chlorites in Japan, with a note on their interference colors. Mineral. J. (Sapporo) 2, 209–223 (1958)
Shirozu, H., Skasegawa, T., Katsumoto, N.: Mg-chlorite and interstratified Mg-chlorite/saponite associated with Kuroko deposits. Clay Sci. 4, 305–321 (1975)
Suzuoki, T., Epstein, S.: Hydrogen isotope fractionation between OH-bearing silicate minerals and water (in preprint form). Publ. Div. Geol. Planet. Sci. Calif. Inst. Tech., Contribution No. 1921 (1970)
Suzuoki, T., Epstein, S.: Partition of hydrogen isotopes between hydrous silicate minerals and water [in Japanese]. Chikyukagaku 5, 38–44 (1972)
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Kuroda, Y., Suzuoki, T., Matsuo, S. et al. A preliminary study of D/H ratios of chlorites. Contr. Mineral. and Petrol. 57, 223–225 (1976). https://doi.org/10.1007/BF00405227
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DOI: https://doi.org/10.1007/BF00405227