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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
https://shinshu.repo.nii.ac.jp/records/43067
https://shinshu.repo.nii.ac.jp/records/4306747ba7a25-cb36-4d28-a410-d7f3a2e2cffd
名前 / ファイル | ライセンス | アクション |
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https://soar-ir.repo.nii.ac.jp/?action=repository_action_common_download&item_id=19799&item_no=1&attribute_id=65&file_no=1
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Item type | Departmental Bulletin Paper(1) | |||||
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公開日 | 2020-09-04 | |||||
タイトル | ||||||
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 | |||||
その他(別言語等)のタイトル | ||||||
その他のタイトル | 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 | |||||
作成者(その他言語) |
日色, 知也
× 日色, 知也× 原山, 智 |
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公開者(その他言語) | ||||||
姓名 | The Faculty of Science, Shinshu University | |||||
書誌情報 |
Journal of the Faculty of Science Shinshu University 巻 47, p. 9-24, 発行日 2018-03-30 |
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言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | resedimentation | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | welded tuff | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | large pyroclastic deposit | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | stratigraphy | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Omine Belt | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Northern Fossa Magna | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
アクセス権 | ||||||
アクセス権 | metadata only access | |||||
アクセス権URI | http://purl.org/coar/access_right/c_14cb | |||||
内容記述 | ||||||
内容記述タイプ | Other | |||||
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. | |||||
日付 | ||||||
日付 | 2018-04-23 | |||||
日付タイプ | Created | |||||
資源タイプ | ||||||
内容記述タイプ | Other | |||||
内容記述 | Article | |||||
その他の資源識別子 | ||||||
内容記述タイプ | Other | |||||
内容記述 | Journal of the Faculty of Science Shinshu University 47 : 9-24(2018) | |||||
資源識別子URI | ||||||
識別子 | http://hdl.handle.net/10091/00020560 | |||||
識別子タイプ | HDL | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 0583-063x | |||||
処理レコードID(総合目録DB) | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA00697924 | |||||
著者版フラグ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 |