Two types of granitic intrusions in the Hida belt, Japan: Sr isotopic and chemical characteristics of the Mesozoic Funatsu granitic rocks

Author:

Arakawa Yoji

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference63 articles.

1. RbSr 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 RbSr 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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