書誌事項
- タイトル別名
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- Mineralogical Consideraion on the Landslides in Serpentinite Belt
- ジャモンガン ヂスベリ ニ タイスル コウブツガクテキ イチ コウサツ
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Many landslides have occured at the serpentinite belt. Mineralogical characteristics of the serpentinite related to the landslides are investigated. The observation by a light microscope and X-ray analysis were carried out. The serpentinite involved a serpentine, brucite and magnetite. The brucite is easily subject to the chemical weathering. As the serpentinite is very fragile, the slope failure occurs easily. The magnetite is stable to the chemical weathering and the serpentine don't change into the clay minerals. So the gentle slope in the serpentinite belt don't slide. Many landslides have occured at the edge of the serpentinite belto.
収録刊行物
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- 地すべり
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地すべり 35 (3), 15-23_1, 1998
公益社団法人 日本地すべり学会
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詳細情報 詳細情報について
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- CRID
- 1390282679522125568
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- NII論文ID
- 10013624805
- 10012529979
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- NII書誌ID
- AN00332562
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- ISSN
- 18843956
- 02852926
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- NDL書誌ID
- 6354080
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- データソース種別
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- JaLC
- NDL
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- 抄録ライセンスフラグ
- 使用不可