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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/10191/39013ca2fd888-f23f-416d-9f5b-8d60378b0d30
名前 / ファイル | ライセンス | アクション |
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4_65-75.pdf (780.2 kB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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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 |
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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 |
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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 |