国鉄新幹線由比ずい道の地質とその応用地質学的解釈
書誌事項
- タイトル別名
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- General and engineering geology of Yui tunnel, Shin-Tokaido Line
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説明
Underground condition of constructing a tunnel is strongly controlled by geological features such as kinds of rocks, geological structure, etc.An example, Yui tunnel of Shin-Tokaido line, is shown in this paper.In this case, hardness decreases at the position of anticlinal axis of strata. Mudstone, even crushed into breccia, holds its own impermeability.Underground water is reserved mainly in the compound strata of tuff?breccia and conglomerate, partly above a muds tone layer as a form of perched water. Places of water seepage are well related with the undulation and faulting of these aquifer in the tunnel.
収録刊行物
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- 応用地質
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応用地質 4 (3), 150-155, 1963
一般社団法人 日本応用地質学会
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詳細情報 詳細情報について
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- CRID
- 1390282679072303744
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- NII論文ID
- 130001613544
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- ISSN
- 18840973
- 02867737
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- データソース種別
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- JaLC
- Crossref
- CiNii Articles
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- 抄録ライセンスフラグ
- 使用不可
