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旧期初生的大規模地すべりについて (藤田至則教授退官記念号)
http://hdl.handle.net/10191/39094
http://hdl.handle.net/10191/39094e8bc5d54-ea75-4c01-bc85-2f2c0d28d327
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 | 2016-03-04 | |||||
タイトル | ||||||
タイトル | 旧期初生的大規模地すべりについて (藤田至則教授退官記念号) | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | 旧期初生的大規模地すべりについて (藤田至則教授退官記念号) | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | primary landslide | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | large-scale landslide | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | ancient landslide | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | slide surface | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | slide block | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 初生的地すべり | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 大規模地すべり | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 旧期地すべり | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 地すべり面 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 地すべりブロック | |||||
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 | On the Large-scale Ancient Primary Landslide | |||||
著者 |
高浜, 信行
× 高浜, 信行 |
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著者別名 | ||||||
識別子 | 161575 | |||||
識別子Scheme | WEKO | |||||
姓名 | Takahama, Nobuyuki | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Two large-scale primary landslides have been found to have occurred in the prehistoric age in the Cenozoic Niigata sedimentary basin. They are the Higashi-mushigame primary landslide and the Sakae primary landslide. Their volumes are of the order of 10^8m^3. The surface topography of both slides is characterized by large peripheral amphitheatric fissures which are represented geomorphologically by drainage patterns, and inside cracks with irregular direction and length. The subsurface strata have been blocked in various sizes. Possible primary slide planes are confirmed at a depth of about 80m below the surface by drilling at the Higashi-mushigame primary landslide, and at a depth of about 100m below the surface by observation of the tunnel walls in the Sakae primary landslide. Secondary landslides, smaller in scale, have occurred in the domain of primary ones. Present active slides have a tendency to occur along fissures and cracks of the primary slide, especially in the marginal part of the primary one. Namely, the occurrence of secondary landslides is controlled by the block structure of the primary landslide. Moreover, there are some reports that plans of engineering works have been met with unexpected troubles caused by large-scale primary landslides. It is an important to elucidate actual conditions of large-scale primary landslides for prediction of disasters and developments in mountainous regions. | |||||
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 10, p. 51-59, 発行日 1988-12 |
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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 |