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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. 36

浜名湖西方地域の秩父帯付加コンプレックスから産出した後期古生代および中生代放散虫化石

http://hdl.handle.net/10091/10675
http://hdl.handle.net/10091/10675
6b338ce3-3e24-41d2-9f97-51d8456a2f88
名前 / ファイル ライセンス アクション
Science36-02-03.pdf Science36-02-03.pdf (1.9 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2010-10-06
タイトル
言語 ja
タイトル 浜名湖西方地域の秩父帯付加コンプレックスから産出した後期古生代および中生代放散虫化石
タイトル
言語 en
タイトル Late Paleozoic and Mesozoic radiolarian fossils from the Chichibu Accretionary Complex in the western area of Lake Hamana, central Japan.
言語
言語 jpn
キーワード
主題Scheme Other
主題 Chichibu Terrane
キーワード
主題Scheme Other
主題 radiolaria
キーワード
主題Scheme Other
主題 Permian
キーワード
主題Scheme Other
主題 Triassic
キーワード
主題Scheme Other
主題 Jurassic
キーワード
主題Scheme Other
主題 accretionary complex
キーワード
主題Scheme Other
主題 melange
キーワード
主題Scheme Other
主題 deformation
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
著者 丹羽, 耕輔

× 丹羽, 耕輔

WEKO 36865

丹羽, 耕輔

Search repository
大塚, 勉

× 大塚, 勉

WEKO 36866

大塚, 勉

Search repository
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 36(2): 77-93(2002)
書誌情報 信州大学理学部紀要

巻 36, 号 2, p. 77-93, 発行日 2002-03-29
抄録
内容記述タイプ Abstract
内容記述 The accretionary complex of the Chichibu Terrane in the western Lake Hamana area is divided into three tectonic units (Units A, B and C) on the basis of lithology and structure. Among them, the Units A and B are melanges comprising chert, basalt and limestone blocks and mudstone matrices. The Unit C is an accumulation of large-scale rock slabs of limestone and basalt. The Units A and C are characterized by horizontal accumulation structure of the slabs and well-developed cleavage. Although the Unit B steeply inclines in usual, rocks of the unit show less deformation than other units. Late Middle and late Middle to early Late Jurassic radiolarians are obtained from chert and siliceous mudstone respectively in the Unit A. Chert of the Unit B yields Early Permian and Middle Triassic radiolarians. Middle to late Middle Jurassic radiolarians are found in mudstone and other pelitic rocks of the Unit B. The fossile evidences suggest that the Unit A is correlative with the Togano Unit of the Southern Chichibu Terrane in radiolarian age.
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
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
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