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The Triassic Tandodani Formation in the Hongo area, Hida Gaien belt, central Japan
https://doi.org/10.18999/joueps.52.1
https://doi.org/10.18999/joueps.52.161976dcc-6603-427f-b0b0-7894cd3a1df5
名前 / ファイル | ライセンス | アクション |
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2007-04-10 | |||||
タイトル | ||||||
タイトル | The Triassic Tandodani Formation in the Hongo area, Hida Gaien belt, central Japan | |||||
言語 | en | |||||
著者 |
Tsukada, Kazuhiro
× Tsukada, Kazuhiro× Niwa, Kohsuke |
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アクセス権 | ||||||
アクセス権 | open access | |||||
アクセス権URI | http://purl.org/coar/access_right/c_abf2 | |||||
抄録 | ||||||
内容記述 | The Triassic Tandodani Formation in the Hongo area, Hida Gaien belt, central Japan is newly defined and described. The formation is divided into the Lower and Upper Members. The former is composed mainly of tuffaceous clastic rocks with minor amount of felsic tuff intercalations, while the latter is mainly felsic tuff, and alternating beds of felsic tuff and tuffaceous mudstone. The Upper Member yields late Triassic conodonts (Tsukada et al., 1997) and, at its upper limit, in in fault contact with the Carboniferous Arakigawa Formation. | |||||
言語 | en | |||||
内容記述タイプ | Abstract | |||||
内容記述 | ||||||
内容記述 | 国立情報学研究所で電子化したコンテンツを使用している。 | |||||
言語 | ja | |||||
内容記述タイプ | Other | |||||
出版者 | ||||||
言語 | en | |||||
出版者 | Dept. of Earth and Planetary Sciences, Nagoya University | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | departmental bulletin paper | |||||
出版タイプ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
ID登録 | ||||||
ID登録 | 10.18999/joueps.52.1 | |||||
ID登録タイプ | JaLC | |||||
ISSN(print) | ||||||
収録物識別子タイプ | PISSN | |||||
収録物識別子 | 0919-875X | |||||
書誌情報 |
en : The Journal of earth and planetary sciences, Nagoya University 巻 52, p. 1-10, 発行日 2005 |
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フォーマット | ||||||
application/pdf | ||||||
著者版フラグ | ||||||
値 | publisher | |||||
URI | ||||||
識別子 | http://hdl.handle.net/2237/7645 | |||||
識別子タイプ | HDL |