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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4号

新潟平野周辺地域における最終氷期最盛期頃の河床下刻作用と地盤隆起運動

http://hdl.handle.net/10191/39013
http://hdl.handle.net/10191/39013
ca2fd888-f23f-416d-9f5b-8d60378b0d30
名前 / ファイル ライセンス アクション
4_65-75.pdf 4_65-75.pdf (780.2 kB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2016-03-03
タイトル
タイトル 新潟平野周辺地域における最終氷期最盛期頃の河床下刻作用と地盤隆起運動
タイトル
言語 en
タイトル 新潟平野周辺地域における最終氷期最盛期頃の河床下刻作用と地盤隆起運動
言語
言語 jpn
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
その他のタイトル
その他のタイトル Downward erosion of river bed and upheaval movement at the maximum Wurm stage around the Niigata Plain, Central Japan
著者 高浜, 信行

× 高浜, 信行

WEKO 162060

高浜, 信行

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著者別名
識別子 162061
識別子Scheme WEKO
姓名 Takahama, Nobuyuki
抄録
内容記述タイプ Abstract
内容記述 The lowest sea level at the maximum Wurm stage was estimated to be 140 meters lower than that at the present time around the Japanese Islands (MINATO, 1966). The strong downward erosin of river bed might have been progressed due to the lowering of the base level. The author investigate the upper limit of the above influence at the maximum Wurm stage, drawing the longitudinal profile of river bed along the middle and lower reaches of the river Shinano. It is presumed, from the investigation that, there might have occurred「knick point」or discontinuity of gradient of the river Shinano at nearby Ojiya city. It is consequently inferred that, direct downward erosion due to the lowering of the sea level along the river Shinano might have attained up to the vicinity Ojiya City. The discontinuity can be attributed mainly to the Neotectonic movement. The downward erosion of the upper stream above the discontinuity would be caused mainly to the upheaval movement. Namely, the mass movement activity along the river Shinano which occurred in upper stream area above Ojiya City would not be effected by the lowering sea level at the maximum Wurm stage, but might have caused mainly due to the upheaval movement.
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 4, p. 65-75, 発行日 1982-11
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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