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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. 47

長野県大町市,大峰帯中部地域の下部更新統の層序と大規模火砕流堆積物の再堆積性砕屑物

http://hdl.handle.net/10091/00020560
http://hdl.handle.net/10091/00020560
eca32b2a-58ae-42fa-b93b-7a54de1bfb8b
名前 / ファイル ライセンス アクション
Science47-02.pdf Science47-02.pdf (1.7 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2018-04-23
タイトル
言語 ja
タイトル 長野県大町市,大峰帯中部地域の下部更新統の層序と大規模火砕流堆積物の再堆積性砕屑物
タイトル
言語 en
タイトル Stratigraphy of the lower-Pleistocene strata and reworking clastic material supplied from large-scale pyroclastic flow deposit in central Omine Belt, Omachi City, Nagano Prefecture, central Japan
言語
言語 jpn
キーワード
言語 en
主題Scheme Other
主題 resedimentation
キーワード
言語 en
主題Scheme Other
主題 welded tuff
キーワード
言語 en
主題Scheme Other
主題 large pyroclastic deposit
キーワード
言語 en
主題Scheme Other
主題 stratigraphy
キーワード
言語 en
主題Scheme Other
主題 Omine Belt
キーワード
言語 en
主題Scheme Other
主題 Northern Fossa Magna
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
著者 日色, 知也

× 日色, 知也

WEKO 105478

ja 日色, 知也

Search repository
原山, 智

× 原山, 智

WEKO 105479

ja 原山, 智

Search repository
信州大学研究者総覧へのリンク
氏名 原山, 智
URL http://soar-rd.shinshu-u.ac.jp/profile/ja.uNTFOUkh.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 Journal of the Faculty of Science Shinshu University 47 : 9-24(2018)
書誌情報 Journal of the Faculty of Science Shinshu University

巻 47, p. 9-24, 発行日 2018-03-30
抄録
内容記述タイプ Abstract
内容記述 The Omine Belt is located in the western margin of the Northern Fossa Magna. Western limit of the Omine Belt is the Itoigawa-Sizuoka Tectonic Line and the eastern limit is the Otari-Nakayama Fault. In the central Omine Belt, Omine Group is interbedded with six volcaniclastic beds from lower to upper stratigraphic following order, Nyunomi Formation, Sonehara Formation,Takagariyama TuffI Member,Takagariyama TuffII Member,Reishoji TuffMember and Omine Formation. After Takagariyama Tuff I Member (1.76 Ma) and Takagariyama Tuff II Member (1.75 Ma) emplaced, the denudation and resedimentation systems have been developed.The systems reflect solidification degree of these pyroclastic flow deposits. Nyukawa Pyroclastic Flow Deposit (Takagariyama TuffI Member)is mostly composed of welded tuff, and Ebisutoge Pyroclastic Deposit (Takagariyama TuffII Member) is composed of nonwelded tuff. Clastic materials derived from Ebisutoge Pyroclastic Deposit are found only at a slightly upper level of the Takagariyama TuffII Member.On the other hand, clastic materials derived from Nyukawa Pyroclastic Flow Deposit are found many horizons in upper beds of the Takagariyama TuffI Member and II.It might be stated that resedimentaion system for the Nyukawa Pyroclastic Flow Deposit continued for a long time because of its welding properties and denudation difficulty.
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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