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Stable isotopic studies on the origin of magnesite deposits in the Setogawa Group, Shizuoka, central Japan(MEMORIAL VOLUME TO THE LATE PROFESSOR TERUHIKO SAMESHIMA)
https://doi.org/10.14945/00000320
https://doi.org/10.14945/00000320cc1381ba-b466-4273-9672-97118c925227
名前 / ファイル | ライセンス | アクション |
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KJ00000102368.pdf (732.6 kB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||||
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公開日 | 2008-01-25 | |||||||
タイトル | ||||||||
言語 | en | |||||||
タイトル | Stable isotopic studies on the origin of magnesite deposits in the Setogawa Group, Shizuoka, central Japan(MEMORIAL VOLUME TO THE LATE PROFESSOR TERUHIKO SAMESHIMA) | |||||||
言語 | ||||||||
言語 | eng | |||||||
キーワード | ||||||||
言語 | en | |||||||
主題Scheme | Other | |||||||
主題 | carbon and oxygen isotopes | |||||||
キーワード | ||||||||
言語 | en | |||||||
主題Scheme | Other | |||||||
主題 | magnesite | |||||||
キーワード | ||||||||
言語 | en | |||||||
主題Scheme | Other | |||||||
主題 | serpentinite | |||||||
キーワード | ||||||||
言語 | en | |||||||
主題Scheme | Other | |||||||
主題 | Setogawa Group | |||||||
資源タイプ | ||||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||||
資源タイプ | departmental bulletin paper | |||||||
ID登録 | ||||||||
ID登録 | 10.14945/00000320 | |||||||
ID登録タイプ | JaLC | |||||||
著者 |
Wada, Hideki
× Wada, Hideki
WEKO
188
× Ohashi, Fumio× Fujioka, Kantaro |
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書誌情報 |
Geoscience reports of Shizuoka University 巻 20, p. 167-173, 発行日 1994-03 |
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出版者 | ||||||||
出版者 | Shizuoka University. Institute of Geosciences | |||||||
NDC | ||||||||
主題Scheme | NDC | |||||||
主題 | 455 | |||||||
抄録 | ||||||||
内容記述タイプ | Abstract | |||||||
内容記述 | Massive magnesite deposits in the Setogawa Group in Shizuoka were formed by an extensive carbonation of serpentinite in an ancient accretionary prism. Stable isotopic investigations of the origin of massive magnesite deposits revealed that a homogeneous deep-seated magmatic carbon mixing with marine limestones may be the main source of the carbon. Many calcite and dolomite veins occur in the serpentines, basaltic and pelitic rocks and based upon carbon and oxygen isotopes are supposed to be of similar origin to carbonate veins found in modern serpentine diapirs of the Izu-Bonin and Mariana is-land arc. In contrast, massive magnesite deposits were formed during the subduction of an active volcano and/or an active ridge, with circulation of magmatic carbon providing the carbon source for the serpentine diapirs. | |||||||
ISSN | ||||||||
収録物識別子タイプ | ISSN | |||||||
収録物識別子 | 03886298 | |||||||
NII論文ID | ||||||||
関連タイプ | isIdenticalTo | |||||||
識別子タイプ | NAID | |||||||
関連識別子 | 110000413355 | |||||||
NII書誌ID | ||||||||
収録物識別子タイプ | NCID | |||||||
収録物識別子 | AN00103190 | |||||||
フォーマット | ||||||||
内容記述タイプ | Other | |||||||
内容記述 | application/pdf | |||||||
著者版フラグ | ||||||||
出版タイプ | VoR | |||||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 |