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General and engineering geology of Yui tunnel, Shin-Tokaido Line
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- Kuroda Kazuo
- 通産省地質調査所
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- Shirai Keiji
- 国鉄静岡幹線工事局
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- Yoshikawa Keiya
- 国鉄技術研究所
Bibliographic Information
- Other Title
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- 国鉄新幹線由比ずい道の地質とその応用地質学的解釈
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Description
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.
Journal
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- Journal of the Japan Society of Engineering Geology
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Journal of the Japan Society of Engineering Geology 4 (3), 150-155, 1963
Japan Society of Engineering Geology
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Keywords
Details 詳細情報について
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- CRID
- 1390282679072303744
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- NII Article ID
- 130001613544
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- ISSN
- 18840973
- 02867737
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- Data Source
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- JaLC
- Crossref
- CiNii Articles
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- Abstract License Flag
- Disallowed