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長野県小谷村，土沢周辺の地質と地すべり
http://hdl.handle.net/10091/10673
http://hdl.handle.net/10091/1067330c19f9b-5f96-4e45-80aa-1012062b514e
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
Science36-02-02.pdf (929.6 kB)
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| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2010-10-06 | |||||
| タイトル | ||||||
| タイトル | 長野県小谷村，土沢周辺の地質と地すべり | |||||
| 言語 | ja | |||||
| タイトル | ||||||
| タイトル | Geology and Landslides along the River Tsunzawa of Otari Village, northwestern Nagano Prefecture, central Japan | |||||
| 言語 | en | |||||
| 言語 | ||||||
| 言語 | jpn | |||||
| キーワード | ||||||
| 言語 | en | |||||
| 主題Scheme | Other | |||||
| 主題 | Ohdaira Landslide | |||||
| キーワード | ||||||
| 言語 | en | |||||
| 主題Scheme | Other | |||||
| 主題 | Tsunzawa Landslide | |||||
| キーワード | ||||||
| 言語 | en | |||||
| 主題Scheme | Other | |||||
| 主題 | Kuruma Group | |||||
| キーワード | ||||||
| 言語 | en | |||||
| 主題Scheme | Other | |||||
| 主題 | Tsunzawa Gravel | |||||
| 資源タイプ | ||||||
| 資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
| 資源タイプ | departmental bulletin paper | |||||
| 著者 |
森川, 篤平
× 森川, 篤平× 小坂, 共栄× 高浜, 信行× 古川, 昭夫 |
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| 出版者 | ||||||
| 出版者 | 信州大学理学部 | |||||
| 引用 | ||||||
| 内容記述タイプ | Other | |||||
| 内容記述 | 信州大学理学部紀要 36(2): 61-75(2002) | |||||
| 書誌情報 |
信州大学理学部紀要 巻 36, 号 2, p. 61-75, 発行日 2002-03-29 |
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| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | The active landslide of the Ohdaira Landslide is situated along the northern shore of the River Tsunzawa of the Otari Village, northwestern Nagano Prefecture, central Japan. The Ohdaira Landslide's max width is about 400m, the max length is about 750m and the height is about 350m. It is surrounded by the Tsunzawa Landslide. The Tsunzawa Landslide's max width is about 2.5km, the max length is about 1.8km and the height is about 500m. Some linear depressions are present on the head of this landslide. The Ohdaira Landslide is the daughter landslide of the Tsunzawa Landslide. The Lower Jurassic Kuruma Group is distributed along the streams on the middle reaches of the river Himekawa. The bed strikes east-west and dips 30 to 60° south. It shows monocline structure. But this structure is disturbed along the river Tsunzawa by the Tsunzawa Landslide activity. The Tsunzawa Gravel rests unconformably upon the Kuruma Group, furthermore the Shirouma-Oike Volcanic Rocks rests unconformably upon the Tsunzawa Gravel. It is composed of only pebble derived from the Kuruma Group. This layer distributes in this study area. It gives great influence on the landslides around middle reaches of the River Himekawa.They are cause of the Ohdaira Landslide activity. | |||||
| 資源タイプ（コンテンツの種類） | ||||||
| 内容記述タイプ | Other | |||||
| 内容記述 | Article | |||||
| ISSN | ||||||
| 収録物識別子タイプ | PISSN | |||||
| 収録物識別子 | 0583-063X | |||||
| 書誌レコードID | ||||||
| 収録物識別子タイプ | NCID | |||||
| 収録物識別子 | AA00697923 | |||||
| 出版タイプ | ||||||
| 出版タイプ | VoR | |||||
| 出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
