Genesis of Late Cretaceous-Paleogene Granitoids with Contrasting Chemical Trends in the Chubu District, Central Japan
Author:
Affiliation:
1. Institute of Geoscience, GSJ
2. Rio Tinto Mining & Exploration Ltd.
Publisher
National Institute of Advanced Industrial Science
Subject
General Medicine
Reference38 articles.
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3. Chappell, B. W. and White, A. J. R. (1992) I and S-type granites in the Lachlan fold Belt. Trans. Royal Soc. Edingburgh: Earth Sci., 83, 1-26.
4. Charoy, B., Couturie, J. P., Raimbault, L. and Liu, Y. (1987) The Suzhou granite complex (East China): Evolution from granite to biotitite with consequent Zr and REE mineralization. Abst. Intern. Sym. “Petrogenesis and Mineralizations of Granitoids”. Inst. Geochem. (Guiyang)ー22-23.
5. Collins, W.J., Beams, S.D., White, A.J.R. and Chappell, B.W. (1982) Nature and origin of A-type granites with particular reference to southwestern Australia. Contrib. Mineral. Petrol., 80, 189-200.
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