Subsurface geology and aquifer system of the Nohbi Plain, central Japan

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.

Bibliographic Details
Main Authors: T. Makinouchi, Tokai Three-Prefecture Investigation Committee on Land Subsidence
Format: Article
Language:English
Published: Copernicus Publications 2015-11-01
Series:Proceedings of the International Association of Hydrological Sciences
Online Access:https://www.proc-iahs.net/372/169/2015/piahs-372-169-2015.pdf
Description
Summary: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.
ISSN:2199-8981
2199-899X