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福井県南条山地北西部,美濃帯の複成的石灰岩礫岩から産出した上部三畳系石灰岩礫
http://hdl.handle.net/10098/00028852
http://hdl.handle.net/10098/00028852b04328e2-f1a4-4559-8cc2-08938a0e5acf
名前 / ファイル | ライセンス | アクション |
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BD10126034 (4.5 MB)
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(c)一般社団法人日本地質学会
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Item type | 学術雑誌論文 / Journal Article(1) | |||||
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公開日 | 2021-12-02 | |||||
タイトル | ||||||
タイトル | 福井県南条山地北西部,美濃帯の複成的石灰岩礫岩から産出した上部三畳系石灰岩礫 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Upper Triassic limestone clasts of the polymictic limestone conglomerate in the Mino Belt, the northwestern Nanjo Mountains, Fukui Prefecture, central Japan | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Mino Belt | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Nanjo Mountains | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | polymictic limestone conglomerate | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Late Triassic | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Imogadaira | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_1843 | |||||
資源タイプ | other | |||||
著者 |
中川, 登美雄
× 中川, 登美雄× 佐野, 弘好× 上松, 佐知子× 指田, 勝男× 渡辺, 幸雄 |
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抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | This paper describes Upper Triassic lime-stone clasts of the polymictic limestone conglomerate (Imogadaira Limestone) of the Mino Belt in the Nanjo Mountains, Fukui Prefecture, central Japan. The Imogadaira Limestone occurs as an isolated block in the Middle Jurassic mélange unit in the upper reaches of the Imogadaira River, Nanjo Mountains. The forma-tion exhibits a prevailing conglomerate fabric, charac-terized by dense packing of limestone clasts within a sparse matrix. The Imogadaira Limestone has a poly-mictic clast association, dominated by Permian lime-stones with lime mudstone and limestone clasts con-taining thin-shelled bivalves. Neither terrigenous clastic grains nor rock fragments occur in the Imogad-aira Limestone. Late Triassic conodonts and Late Tri-assic and Early Jurassic radiolarians were extracted from whole-rock samples of the Imogadaira Limestone. Further examination revealed that the Late Triassic conodonts and radiolarians occurred within limestone clasts containing thin-shelled bivalves. |
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書誌情報 |
地質学雑誌 en : J. Geol. Soc. Japan 巻 125, 号 12, p. 877-884, 発行日 2019-12 |
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出版者 | ||||||
出版者 | 一般社団法人日本地質学会 | |||||
DOI | ||||||
関連タイプ | isIdenticalTo | |||||
識別子タイプ | DOI | |||||
関連識別子 | 10.5575/geosoc.2019.0033 | |||||
権利 | ||||||
権利情報 | (c)一般社団法人日本地質学会 | |||||
関連サイト | ||||||
識別子タイプ | URI | |||||
関連識別子 | https://www.jstage.jst.go.jp/article/geosoc/125/12/125_2019.0033/_article/-char/ja | |||||
関連名称 | 地質学雑誌 | |||||
著者版フラグ | ||||||
出版タイプ | AO | |||||
出版タイプResource | http://purl.org/coar/version/c_b1a7d7d4d402bcce | |||||
その他のID | ||||||
TD10126034 |