Geographical Characteristics and Sources of Dissolved Ions in Groundwater at the Southern Part of Mt. Fuji-Reference-Cited by-同舟云学术

Geographical Characteristics and Sources of Dissolved Ions in Groundwater at the Southern Part of Mt. Fuji

Published:2017 Issue:1 Volume:126 Page:43-71
ISSN:0022-135X
Container-title:Journal of Geography (Chigaku Zasshi)
language:en
Short-container-title:Journal of Geography(Chigaku Zasshi)

Author:

KAMITANI Takafumi¹,WATANABE Masayuki¹,MURANAKA Yasuhide¹,SHIN Ki-cheol²,NAKANO Takanori²

Affiliation:

1. Shizuoka Institute of Environment and Hygiene

2. Research Institute for Humanity and Nature

Publisher

Tokyo Geographical Society

Subject

Materials Chemistry

Link

https://www.jstage.jst.go.jp/article/jgeography/126/1/126_126.43/_pdf

Reference49 articles.

1. Berner, E.K. and Berner, R.A. (1987): The Global Water Cycle. Prentice-Hall: Englewood Cliffs.

2. Faure, G. (1991): Principles and Applications of Inorganic Geochemistry. Macmillan Coll. Div.

3. Fujii, T. (2004): Why does basalt magma excel in the Fuji volcano?. Chikyu Monthly Symposium, 48, 153-159.*

4. Fujii, T. and Yui, M. (2004): Characteristics of the lithology of the Ashitaka volcano. Earth Monthly, 7, 622-627.*

5. Fujimura, I. (1971): The climate and weather of Mt. Fuji. in Results of the Co-operative Scientific Survey of Mt. Fuji. Fuji-san (Fujisan: Fujisan Sogo Gakujutsu Chosa Hokokusho) edited by National Park Association of Japan, Fuji Kyuko, 211-345.

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