Two types of granitic intrusions in the Hida belt, Japan: Sr isotopic and chemical characteristics of the Mesozoic Funatsu granitic rocks
Author:
Publisher
Elsevier BV
Subject
Geochemistry and Petrology,Geology
Reference63 articles.
1. RbSr ages of the gneiss and metamorphosed intrusive rocks of the Hida metamorphic belt in the Urushiyama area, Gifu Prefecture, central Japan;Arakawa;J. Jpn. Assoc. Mineral. Petrol. Econ. Geol.,1984
2. Structural and geochemical development of the Hida metamorphic complex, central Japan;Arakawa,1985
3. Two contrasting types of RbSr isotope systems for the Funatsu granitic rocks in the northwestern part of the Hida belt, central Japan;Arakawa;J. Mineral. Petrol. Econ. Geol.,1988
4. Profile of initial 87Sr86Sr ratios for the Funatsu granitic rocks in the western part of the Hida belt;Arakawa,1988
5. Relationship between shear zones and Sr isotope compositions of granitic rocks in the Hida belt;Arakawa;Japan. J. Geol.,1990
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