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Mid-Tertiary magmatic events in New Caledonia : K-Ar dating of boninitic volcanism and granitoid(MEMORIAL VOLUME TO THE LATE PROFESSOR TERUHIKO SAMESHIMA) intrusives
https://doi.org/10.14945/00000318
https://doi.org/10.14945/00000318d0c36083-f440-403c-9725-a54f70a71f0a
名前 / ファイル | ライセンス | アクション |
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KJ00000102358.pdf (637.7 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 | Mid-Tertiary magmatic events in New Caledonia : K-Ar dating of boninitic volcanism and granitoid(MEMORIAL VOLUME TO THE LATE PROFESSOR TERUHIKO SAMESHIMA) intrusives | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | boninite | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | clinoenstatite | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | ultramafics | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | granodiorites | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | New Caledonia | |||||
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 | 10.14945/00000318 | |||||
ID登録タイプ | JaLC | |||||
著者 |
Black, Philippa M.
× Black, Philippa M.× Itaya, Tetsumaru× Ohira, Takashi× Smith, Ian E. M.× Takagi, Miki |
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書誌情報 |
Geoscience reports of Shizuoka University 巻 20, p. 49-53, 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 | 453 | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | The Cenozoic geological record of New Caledonia contains two autochthonous magmatic associations, the Early Eocene Formation of Basalts and the . Late Oligocene-Early Miocene granitoid suite of the Koum and St Louis areas. New K-Ar dates show that the boninites in the Nepoui region, hitherto thought to be Early Eocene, are Late Oligocene. Allochthonous ultramafic rocks of the New Caledonia Ophiolite were emplaced in the Late Eocene or Early Oligocene. The similar age of the Nepoui boninites and the Koum-St Louis granitoids suggests that they were linked to a short lived subduction event which took place after ophiolite emplacement. | |||||
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 | 110000413345 | |||||
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 |