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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

イライト結晶度からみた長野県諏訪湖南方における三波川帯・秩父帯・四万十帯の弱変成作用

http://hdl.handle.net/10091/10671
http://hdl.handle.net/10091/10671
12a3b26c-55dd-4a32-ac1c-8849a538eb7e
名前 / ファイル ライセンス アクション
Science35-01-02.pdf Science35-01-02.pdf (3.3 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 イライト結晶度からみた長野県諏訪湖南方における三波川帯・秩父帯・四万十帯の弱変成作用
タイトル
言語 en
タイトル Illite crystallinlty and Low-grade metamorphism of the Sanbagawa, Chichibu and Shinianto Belts in the south area of Lake Suwa, central Japan.
言語
言語 jpn
キーワード
言語 en
主題Scheme Other
主題 illite crystallinity
キーワード
言語 en
主題Scheme Other
主題 Kubler index
キーワード
言語 en
主題Scheme Other
主題 Sanbagawa Belt
キーワード
言語 en
主題Scheme Other
主題 Chichibu Belt
キーワード
言語 en
主題Scheme Other
主題 Shimanto Belt
キーワード
言語 en
主題Scheme Other
主題 Todai Formation
キーワード
言語 en
主題Scheme Other
主題 Sanbagawa metamorphism
キーワード
言語 en
主題Scheme Other
主題 contact metamorphism
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 金本, 高明

× 金本, 高明

WEKO 36880

ja 金本, 高明

Search repository
大塚, 勉

× 大塚, 勉

WEKO 36881

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 35(1): 11-29(2000)
書誌情報 信州大学理学部紀要

巻 35, 号 1, p. 11-29, 発行日 2000-10-30
抄録
内容記述タイプ Abstract
内容記述 The illite crystallinity (Kubler index) was measured for the pelitic rocks from the Sanbagawa, Chichibu and Shimanto Belts in the south area of Lake Suwa, centralJapan. These belts are composed of the complexes formed through subduction- and accretion-related processes and they are characterized by the effects of high-pressure and low-temperature type metamorphism and deformation. Early Cretaceous Todai Formation is exposed in the narrow zone along the boundary faults between the Sanbagawa and Chichibu Belts. The illite crystallinity for the rocks from the Sanbagawa and Chichibu Belts corresponds to that of the higher part of the anchizone to lower part of the epizone, while that from the Todai Formation shows a range from the lower to the higher part of the anchizone. The burial metamorphism for the Sanbagawa, Chichibu Belt and the Todai Formation increases from the south to the north gradually. This fact indicates that the relatively deeper part of the complexes became exposed to the earth's surface in the northern part of the study area. It is inferred that the metamorphism recorded in the Todai Formation is correlated with the Sanbagawa metamorphism considering the depositional age of the formation.
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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