Chemical contrast of the Late Cretaceous granitoids of the Sanyo and Ryoke Belts, Southwest Japan: Okayama-Kagawa Transect.-Reference-Cited by-同舟云学术

Chemical contrast of the Late Cretaceous granitoids of the Sanyo and Ryoke Belts, Southwest Japan: Okayama-Kagawa Transect.

Published:2003 Issue:3-4 Volume:54 Page:95-116
ISSN:1346-4272
Container-title:BULLETIN OF THE GEOLOGICAL SURVEY OF JAPAN
language:en
Short-container-title:Bull. Geol. Surv. Japan

Author:

Ishihara Shunso¹

Affiliation:

1. Geological Survey of Japan, AIST

Publisher

National Institute of Advanced Industrial Science

Subject

General Medicine

Reference26 articles.

1. Champion, D. C. and Chappell, B. W. (1992) Petrogenesis of felsic I-type granites; An example from northern Queensland. Trans. Royal Soc. Edingburgh: Earth Sci., 83, 115-126.

2. Hida, N., Shimazu, M. and Igarashi, T. (1961) Granitic rocks and related uranium metallic ore deposits in Sanyo District. In Natural Occurrence of Uranium in Japan. Rept. Geol. Surv. Japan no. 190, 68-79 (in Japanese with English abstract).

3. Ishihara, S. (1971) Modal and chemical compositions of the granitic rocks related to the major molybdenum and tungsten deposits in the Inner Zone of Southwest Japan. Jour. Geol. Soc. Japan, 77, 441-452.

4. Ishihara, S. (1991) The Aji stone: The historical and modern use and its geologic background. Chishitsu News, no. 441, 60-67 (in Japanese).

5. Ishihara, S. (2002) Chemical characteristics of the mineralized granitoids (I). Mo and W provinces of the Inner Zone of Southwest Japan. Bull. Geol. Surv. Japan, 53, 657-671 (in Japanese with English abstract).

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