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  1. 040 理学部
  2. 0401 学術論文

琵琶湖深層ボーリング資料からみた近江盆地の構造運動と堆積環境

http://hdl.handle.net/10091/12277
fd70bd89-e7c0-40d8-b76e-121fd3714a34
名前 / ファイル ライセンス アクション
lakebiwamuseum_12-02.pdf lakebiwamuseum_12-02.pdf (955.3 kB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2011-04-14
タイトル
言語 ja
タイトル 琵琶湖深層ボーリング資料からみた近江盆地の構造運動と堆積環境
言語
言語 jpn
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 Tectonic movements and sedimentary environments of Omi basin deduced from the deep drillings around Lake Biwa, Japan
著者 公文, 富士夫

× 公文, 富士夫

WEKO 36313

公文, 富士夫

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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 滋賀県立琵琶湖博物館
引用
内容記述タイプ Other
内容記述 琵琶湖博物館研究調査報告. 12:155-162 (1999)
書誌情報 琵琶湖博物館研究調査報告

巻 12, p. 155-162, 発行日 1999-05
抄録
内容記述タイプ Abstract
内容記述 The sinking rates of the different parts of Lake Biwa can be calculated based on the marker tephras and their depth in the four deep drillings in and near the lake. Two sites of the drilling have high sinking rate as large as 0.8mm/year, and other two sites have slow rates as large as 0.5mm/year. On the other hand, modem structural units in the Omi basin can be estimated by the topography, geology and active fault systems. There exist many small quadrilateral units of which sides are as long as a few kilometers in the Omi basin. New tectonic movement started about 400,000years ago, and the differential sinking of the structural units have been played a basic roll to form the present Omi sedimentary basin and its topography which include Lake Biwa. Strong subsidence and poor sediment supply formed deep water environment such as northern Iake of Lake Biwa., and weak sinking or strong sinking with abundant sediment supply caused the shalIow lake or fIuvial environments for a Iong time such as southern lake of Lake Biwa and Koto plain, east-side plain of Lake Biwa.
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
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AA11293380
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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