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  1. 0 資料タイプ別
  2. 03 紀要論文
  1. 360 災害・復興科学研究所
  2. 20 紀要
  3. 90 新潟大学積雪地域災害研究センター研究年報
  4. 第7号

Mass movement in the eastern margin of the cenozoic Niigata sedimentary basin, central Japan : its geohistorical backgrounds

http://hdl.handle.net/10191/39062
http://hdl.handle.net/10191/39062
21814a46-4c0a-4bfb-8195-dc98e49aabb3
名前 / ファイル ライセンス アクション
7_7-72.pdf 7_7-72.pdf (5.3 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2016-03-03
タイトル
タイトル Mass movement in the eastern margin of the cenozoic Niigata sedimentary basin, central Japan : its geohistorical backgrounds
タイトル
言語 en
タイトル Mass movement in the eastern margin of the cenozoic Niigata sedimentary basin, central Japan : its geohistorical backgrounds
言語
言語 eng
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
著者 Takahama, Nobuyuki

× Takahama, Nobuyuki

WEKO 161837

Takahama, Nobuyuki

Search repository
抄録
内容記述タイプ Abstract
内容記述 The geohistorical investigation has been made on the two different kinds of large-scale mass movements in the eastern marginal region of the Niigata Sedimentary basin, i.e., the Gozu debris flows and the Aburuma-gawa landslides. The stratigraphic successions of these mass movement deposits show the following important characteristics common to the both. 1) These mass movements have occurred repeatedly at nearly the same sites since the Middle Pleistocene to the present. 2) During Middle Pleistocene and early Late Pleistocene time, the large-scale debris flows and the primary landslide occurred almost contemporaneously with the development of the mountain topography. The origin and development of these mass movements have been strongly controlled by the crustal movements since Middle Pleistocene time. The amount of upheaval of the Gozu Mountains in this period have reached about 1,000 m in maximum height. The rapid block upheaval of the Gozu Mountains and the Uonuma Hills with an increasing elevation had brought about the fracturing and collapse associated with faulting and successive erosive rejuvenation, and finally resulted in generation of the large-scale mass movements. The sea level lowering and periglacial process in the glacial epoch are not essential for the origin of mass movement in the region studied.
書誌情報 新潟大学積雪地域災害研究センター研究年報
en : 新潟大学積雪地域災害研究センター研究年報

巻 7, p. 7-72, 発行日 1986-01
出版者
出版者 新潟大学積雪地域災害研究センター
ISSN
収録物識別子タイプ ISSN
収録物識別子 03877892
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AN00183327
著者版フラグ
値 publisher
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