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  1. 040 理学部
  2. 0402 紀要
  3. 04021 Journal of the Faculty of Science, Shinshu University
  4. Vol. 35

美濃帯味噌川コンプレックスのチャートおよび珪質泥岩から産出したジュラ紀中世および新世の放散虫化石群集

http://hdl.handle.net/10091/10668
b3c8dcfa-9ee4-4c32-82f6-b3351282a7f1
名前 / ファイル ライセンス アクション
Science35-02-03.pdf Science35-02-03.pdf (2.9 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2010-10-06
タイトル
タイトル 美濃帯味噌川コンプレックスのチャートおよび珪質泥岩から産出したジュラ紀中世および新世の放散虫化石群集
言語
言語 jpn
キーワード
主題Scheme Other
主題 Mino Terrane
キーワード
主題Scheme Other
主題 Misogawa Complex
キーワード
主題Scheme Other
主題 Middle Jurassic
キーワード
主題Scheme Other
主題 Late Jurassic
キーワード
主題Scheme Other
主題 radiolarians
キーワード
主題Scheme Other
主題 Stylocapsa(?) spiralis zone
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
その他(別言語等)のタイトル
その他のタイトル Middle to Late Jurassic radiolarian assemblages from chert and siliceous mudstone in the Misogawa Complex of the Mino Terrane, central Japan.
著者 首藤, 拓郎

× 首藤, 拓郎

WEKO 36876

首藤, 拓郎

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大塚, 勉

× 大塚, 勉

WEKO 36877

大塚, 勉

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信州大学研究者総覧へのリンク
氏名 大塚, 勉
URL http://soar-rd.shinshu-u.ac.jp/profile/ja.OmyauUkV.html
出版者
出版者 信州大学理学部
引用
内容記述タイプ Other
内容記述 信州大学理学部紀要 35(2): 79-92(2001)
書誌情報 信州大学理学部紀要

巻 35, 号 2, p. 79-92, 発行日 2001-03-30
抄録
内容記述タイプ Abstract
内容記述 The Misogawa Complex is a Late Jurassic accretionary complex widely exposed in the eastern part of the Mino Terrane, central Japan. The complex is mainly composed of sandstone, mudstone and chert, and they are generally deformed in various degrees. Among the complex, exceptionally well-continuous sequences are exposed along the Nakazawa-gawa River in the Kisofukushima area, Nagano Prefecture. Pelagic chert is conformably covered by hemipelagic siliceous mudstone in the outcrop. Middle to Late Jurassic radiolarian assemblages corresponding to Tricolocapsa plicarum, T. conexa and Stylocapsa(?) spiralis zones (Matsuoka, 1995) were found in the sequence. The radiolarian biohorizon of the top of the chert is correlative with Stylocapsa(?) spiralis zone that ranges from latest Middle to early Late Jurassic. The age of the stratigraphic boundary is interpreted as the arrival time of the oceanic plate at the outer trench where the terrigenous materials were first deposited in the sequence. The age indicated by the radiolarians from the Nakazawa-gawa River sequence is the youngest evidence in the eastern Mino Terrane.
資源タイプ(コンテンツの種類)
内容記述タイプ Other
内容記述 Article
ISSN
収録物識別子タイプ ISSN
収録物識別子 0583-063X
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AA00697923
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