12 Nov 2015
12 Nov 2015
Subsurface geology and aquifer system of the Nohbi Plain, central Japan
T. Makinouchi1 and Tokai Three-Prefecture Investigation Committee on Land Subsidence2
T. Makinouchi and Tokai Three-Prefecture Investigation Committee on Land Subsidence
T. Makinouchi1 and Tokai Three-Prefecture Investigation Committee on Land Subsidence2
- 1Department of Environmental Science and Technology, Faculty of Science and Technology, Meijo University, Nagoya, 468-8502, Japan
- 2Chubu Geographical Survey Institute, Geospatial Information Authority of Japan, Nagoya, 460-0001, Japan
- 1Department of Environmental Science and Technology, Faculty of Science and Technology, Meijo University, Nagoya, 468-8502, Japan
- 2Chubu Geographical Survey Institute, Geospatial Information Authority of Japan, Nagoya, 460-0001, Japan
Correspondence: T. Makinouchi (takmak@meijo-u.ac.jp)
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The Nohbi Plain is a typical coastal plain in Japan. The subsurface of this plain consists of alternating beds of marine clays in transgressive stages and fluvial gravels in regressive stages, and forms a groundwater basin. The aquifers are represented by the gravel beds in the regressive stages.
