Origin of hornblendites in the Oeyama (Komori) ultramafic body in view of hydrogen isotope study

Origin of hornblendites in the Oeyama (Komori) ultramafic body in view of hydrogen isotope study

Hornblendes from epidote-hornblendites in the contact aureole of the younger granite in the Oeyama ultramafic body are concluded to have been formed by recrystallization of clinopyroxenite on the supply of water from the intruding granite. The value of δD of source water is estimated to be -60∼-65 ‰...

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Veröffentlicht in:GEOCHEMICAL JOURNAL 1975/09/20, Vol.9(3), pp.173-176
Hauptverfasser: Kuroda, Yoshimasu, Kinugawa, Tomoyasu, Suzuoki, Tetsuro, Matsuo, Sadao
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container_title GEOCHEMICAL JOURNAL
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creator Kuroda, Yoshimasu
Kinugawa, Tomoyasu
Suzuoki, Tetsuro
Matsuo, Sadao
description Hornblendes from epidote-hornblendites in the contact aureole of the younger granite in the Oeyama ultramafic body are concluded to have been formed by recrystallization of clinopyroxenite on the supply of water from the intruding granite. The value of δD of source water is estimated to be -60∼-65 ‰, which is definitely lower than -29∼-37 ‰ of water in granitic magma of the Kitakami mountainous district.
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title Origin of hornblendites in the Oeyama (Komori) ultramafic body in view of hydrogen isotope study
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