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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. 33

関東山地北縁,下仁田構造帯内部から発見された大北野安山岩

http://hdl.handle.net/10091/10656
http://hdl.handle.net/10091/10656
003132c9-40d7-4946-a9e9-d706a41eb86c
名前 / ファイル ライセンス アクション
Science33-01-03.pdf Science33-01-03.pdf (646.7 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 関東山地北縁,下仁田構造帯内部から発見された大北野安山岩
タイトル
言語 en
タイトル An occurence of the Okitano Andesite in the Shimonita Tectonic Zone of the northern margin of the Kanto Mountains, central Japan
言語
言語 jpn
キーワード
言語 ja
主題Scheme Other
主題 下仁田構造帯
キーワード
言語 ja
主題Scheme Other
主題 中央構造線
キーワード
言語 ja
主題Scheme Other
主題 大北野安山岩
キーワード
言語 ja
主題Scheme Other
主題 瀬戸内火山岩類
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
著者 藤白, 隆司

× 藤白, 隆司

WEKO 36906

ja 藤白, 隆司

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小坂, 共栄

× 小坂, 共栄

WEKO 36907

ja 小坂, 共栄

Search repository
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 33(1): 17-26(1998)
書誌情報 信州大学理学部紀要

巻 33, 号 1, p. 17-26, 発行日 1998-10-30
抄録
内容記述タイプ Abstract
内容記述 The Shimonita Tectonic Zone is one of the important tectonic area running from east to west along the northern marginal area of the Kanto Mountains. A small andesitic body which has intruded into the lower Miocene Shimonita Formation is newly found in the present area. Essential phenocrysts of the Okitano Andesite are plagioclase and pyroxene. The groundmass is microcrystalline in which the plagioclase crystals are oriented. The chemical compositions of major elements are similar to the Setouchi Volcanic Province of southwest Japan. It indicates that the igneous activity which is assinged to the Setouchi Province has happened in the Shimonita Tectonic Zone in age of Miocene time.
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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