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古期土石流の断続的な発生と構造運動 : 五頭土石流の1例
http://hdl.handle.net/10191/39037
http://hdl.handle.net/10191/390376ecdf423-66ec-453d-b11a-21c060bb2926
名前 / ファイル | ライセンス | アクション |
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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 | 古期土石流の断続的な発生と構造運動 : 五頭土石流の1例 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | 古期土石流の断続的な発生と構造運動 : 五頭土石流の1例 | |||||
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 | Relation of intermittent occurrence of older debris flows to block uplift : Gozu debris flow | |||||
著者 |
高浜, 信行
× 高浜, 信行× 野崎, 保 |
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著者別名 | ||||||
識別子 | 161930 | |||||
識別子Scheme | WEKO | |||||
姓名 | Takahama, Nobuyuki | |||||
著者別名 | ||||||
識別子 | 161931 | |||||
識別子Scheme | WEKO | |||||
姓名 | Nozaki, Tamotsu | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Debris flow deposits, that occurred during the Middle Pleistocene to the present, are widely distributed at the western foot of the Gozu Mountains. They are called the Gozu debris flow deposits. The stratigraphy and geohistorical development of debris flows have been outlined by TAKAHAMA and NOZAKI (1981). The Gozu debris flow deposits is divided into the following seven gravel beds in ascending order; GD I and GD II (the Middle Pleistocene), GD III, GD IV and GDV (the Upper Pleistocene) and GD VI and GD VII (the Holocene). The characteristics of the Gozu debris flow development is that the large-scale debris flows occurred intermittently during the Middle Pleistocene and the early Late Pleistocene times, with a long periods of “suspension”. Their deposits are GD I, GD II and GD III. During the “suspending periods”, these gravel beds were weathered intensely and their depositional surface were dissected. The Gozu Mountains made stepped block upheaval, with the maximum uplift amounting to around 1,000 meters since the Middle Pleistocene time up to the present (TAKAHAMA, 1984). The intense faulting and block uplift caused the strong erosive rejuvenation leadig to the intermittent occurrence of large-scale debris flows. | |||||
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 6, p. 53-62, 発行日 1985-01 |
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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 |