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  1. 040 理学部
  2. 0401 学術論文

長野県北西部,青木湖の成因と周辺の最上部第四紀層

http://hdl.handle.net/10091/3718
ba39edf3-ab18-42c9-8bf5-c7ae8e4f80e4
名前 / ファイル ライセンス アクション
daiyonki-39-1.pdf daiyonki-39-1.pdf (1.7 MB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2009-12-08
タイトル
言語 ja
タイトル 長野県北西部,青木湖の成因と周辺の最上部第四紀層
言語
言語 jpn
キーワード
主題Scheme Other
主題 後期更新世
キーワード
主題Scheme Other
主題 完新世
キーワード
主題Scheme Other
主題 青木湖
キーワード
主題Scheme Other
主題 佐野坂丘陵
キーワード
主題Scheme Other
主題 指標テフラ
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ journal article
その他(別言語等)のタイトル
その他のタイトル Late Quaternary Sediments around Lake Aoki,Nagano, Central Japan, and the Origin of the Lake
著者 多, 里英

× 多, 里英

WEKO 36503

多, 里英

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公文, 富士夫

× 公文, 富士夫

WEKO 36504

公文, 富士夫

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小林, 舞子

× 小林, 舞子

WEKO 36505

小林, 舞子

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酒井, 潤一

× 酒井, 潤一

WEKO 36506

酒井, 潤一

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信州大学研究者総覧へのリンク
氏名 公文, 富士夫
URL http://soar-rd.shinshu-u.ac.jp/profile/ja.ZUchOUkh.html
出版者
出版者 日本第四紀学会
引用
内容記述タイプ Other
内容記述 第四紀研究. 39(1):1-13 (2000)
書誌情報 第四紀研究

巻 39, 号 1, p. 1-13, 発行日 2000-02
抄録
内容記述タイプ Abstract
内容記述 青木湖周辺には,後期更新世から完新世にかけての,おもに河成や湖成の堆積物が断片的に分布しており,下位より藪沢層,崩沢層,神城砂磯層,佐野坂崩壊堆積物,青木湖成段丘堆積物,青木湖底堆積物に分けられる,指標テフラと岩相対比によって,それらの相互関係を明らかにした.佐野坂崩壊堆積物の上位には, Dpm火山灰層がのるとされていたが,それを再堆積物と判断し,周辺の地史を次のように推定した.藪沢層は,比較的広い谷の中を南から北へ流れる蛇行河川によって形成された.その時代は5万年前以前の寒冷な時期である.約5万年前,その河川は狭い谷の中を流れる網状河川に変化した.この堆積環境の変化は, DKP火山灰層を挟む崩沢層と神城砂喋層中部が礫疎を主体とすることにより示されている.約3万年前に,西方の仁科山地で大規模な地すべり崩壊が起こり,佐野坂丘陵が形成された.この崩壊堆積物は川をせき止め,丘陵の南側に深い湖(青木湖)を形成した.佐野坂丘陵の北側の凹地には支谷からの堆積物供給が多く,徐々に堆積されて,現在の神城盆地を形成するようになった.
抄録
内容記述タイプ Abstract
内容記述 The late Pleistocene and Holocene sediments around Lake Aoki are divided into the Yabusawa Formation, Kuzuresawa formation,Kamishiro Gravel-sand Formation, Sanosaka Debris Deposits, Aokiko Terrace Deposit, and Aokiko Deposits, on the basis of lithology and tephro-stratigraphic correlation. The Yabusawa Formation and its correlatives are mainly composed of silt with abundant plant remains, deposited in a cold period more than 50,000 years ago. They were formed by a meandering river which flowed from south to north as a relatively wide valley. The gravel sediments of the Kuzuresawa Formation and the middle part of the Kamishiro Gravel-sand Formation were formed by a braided river. A giant landslide took place at the eastern margin of the Nishina Mountains and dammed up the river about 30,000 years ago. This landslide deposits made the Sanosaka Hill.The deep depression in the south is Lake Aoki, which has maintained a deep water condition until the present. The furrow in the north of the hill was filled gradually by a large amount of clastic sediment through river streams, forming the Kamishiro Basin.
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 ISSN
収録物識別子 0418-2642
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AN0034136X
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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