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  1. 040 理学部
  2. 0402 紀要
  3. 04021 Journal of the Faculty of Science, Shinshu University
  4. Vol. 45

Effect of geological structures, rock weathering, and clay mineralogy in the formation of various landslides along Mugling-Narayanghat road section, Central Nepal Himalaya

http://hdl.handle.net/10091/16910
982e3a4b-7ab2-4fd2-b289-4f6fa7317a7e
名前 / ファイル ライセンス アクション
Science45-01.pdf Science45-01.pdf (3.7 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2013-04-02
タイトル
タイトル Effect of geological structures, rock weathering, and clay mineralogy in the formation of various landslides along Mugling-Narayanghat road section, Central Nepal Himalaya
言語
言語 eng
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
著者 REGMI, Amar Deep

× REGMI, Amar Deep

WEKO 36806

REGMI, Amar Deep

Search repository
YOSHIDA, Kohki

× YOSHIDA, Kohki

WEKO 36807

YOSHIDA, Kohki

Search repository
信州大学研究者総覧へのリンク
氏名 YOSHIDA, Kohki
URL http://soar-rd.shinshu-u.ac.jp/profile/ja.umThOUkh.html
出版者
出版者 Faculty of Science, Shinshu University
引用
内容記述タイプ Other
内容記述 Journal of the Faculty of Science Shinshu University 45: 1-44(2013)
書誌情報 Journal of the Faculty of Science Shinshu University

巻 45, p. 1-44, 発行日 2013-03-27
抄録
内容記述タイプ Abstract
内容記述 The present study was conducted on the landslide prone area around Mugling-Narayanghat road section that consists of Lesser Himalayan and Siwaliks rocks. From more than 250 mapped landslides, ten were selected for detailed study that are supposed to the representative of the whole area. Detailed study showed that large and complex landslides are related to deep rock weathering followed by the intervention of geological structures as faults, joints, and fractures. Large landslides formed by gravitational deformation are related to the rock structures, while rock weathering plays a minor role. Rotational types of landslides are observed in weathered rocks, where the dip direction of the foliation plane plays a principle role. Shallow landslides are common in slopes covered by residual soil or colluviums. Some shallow landslides (rock topples) occur in less weathered rocks where the attitude of the foliation plays a major role, while others (rock plane failure) occur in cut slopes with less weathered rocks. Debris slides/flows occur in colluviums or residual soil covered slopes. In few instances, rock fall may occur on the upper slope, which then is mixed with the colluviums, residual soil, and other materials lying downhill and come down as debris flow. Rock falls are mainly related to the joint pattern and the slope angle and are found in less weathered rocks.
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 ISSN
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
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