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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. 32

美濃帯上麻生地域の大規模摺曲の形態と成因

http://hdl.handle.net/10091/10646
http://hdl.handle.net/10091/10646
e2130950-942a-47f0-a0ce-334ed0061c00
名前 / ファイル ライセンス アクション
Science32-01-03.pdf Science32-01-03.pdf (988.7 kB)
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 美濃帯上麻生地域の大規模摺曲の形態と成因
タイトル
言語 en
タイトル Large-scale folds in the Kamiaso area, Mino Terrane, central Japan.
言語
言語 jpn
キーワード
言語 en
主題Scheme Other
主題 Mino Terrane
キーワード
言語 en
主題Scheme Other
主題 Kamiaso
キーワード
言語 en
主題Scheme Other
主題 chert
キーワード
言語 en
主題Scheme Other
主題 fold
キーワード
言語 en
主題Scheme Other
主題 half-dome
キーワード
言語 en
主題Scheme Other
主題 half-basin
キーワード
言語 en
主題Scheme Other
主題 sinistral simple shear
キーワード
言語 en
主題Scheme Other
主題 Cretaceous
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
著者 水野, 真理子

× 水野, 真理子

WEKO 36921

ja 水野, 真理子

Search repository
大塚, 勉

× 大塚, 勉

WEKO 36922

ja 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 32(1): 27-36(1997)
書誌情報 信州大学理学部紀要

巻 32, 号 1, p. 27-36, 発行日 1997-10-29
抄録
内容記述タイプ Abstract
内容記述 The Mino Terrane in central Japan is the Jurassic typical subduction complex. The complex has been folded to form large-scale synclines and anticlines trending E-W and plunging west. Small-scale folds are commonly found in the cherts which are widely exposed in the Mino Terrane. The chert folds are considered to have been formed under the uniform stress field in subduction/accretion in Jurassic time. The regular orientation of the axes of the chert folds can be regarded as an index for analysis of the three-dimensional form of the large-scale synclines and anticlines. Judging from the change of the orientation of the axes of the chert folds, the Shimonoho syncline and the Nakanoho anticline in the Kamiaso area show asymmetrical half-basin and half-dome structures. The asymmetry of the syncline and anticline indicates that they have been formed under the remarkable sinistral simple shear. The large-scale folds are widespread over the pre-Cretaceous terranes in the Southwest Japan. The age of the formation of the large-scale folds are restricted between late Early and early Late Cretaceous time. The formation of the large-scale folds in Cretaceous time is interpreted as a result of the sinistral displacement that dominated the eastern margin of the Eurasian continent.
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 PISSN
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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