Strontium isotopic compositions of Mesozoic granitic rocks in the Hida belt, central Japan: diversities of magma sources and of processes of magma evolution in a continental margin area-Reference-Cited by-同舟云学术

Strontium isotopic compositions of Mesozoic granitic rocks in the Hida belt, central Japan: diversities of magma sources and of processes of magma evolution in a continental margin area

Published:1990-08 Issue:4 Volume:24 Page:261-273
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Arakawa Yoji

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference66 articles.

1. Geologic structures of the Hida metamorphic rocks of the Kurobe and Katakai River areas, in the eastern part of Toyama prefecture, central Japan;Arakawa;Sci. Rep. Inst. Geosci. Univ. Tsukuba,1982

2. RbSr ages of the gneiss and metamorphosed intrusive rocks of the Hida metamorphic belt in the Urushiyama area, Gifu Prefecture, central Japan;Arakawa;J. Jap. Assoc. Mineral. Petrol. Econ. Geol.,1984

3. Structural and geochemical development of the Hida metamorphic complex, central Japan;Arakawa,1985

4. 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

5. Relationship between shear zones and Sr isotope compositions of granitic rocks in the Hida belt;Arakawa;Japan. J. Geology,1990

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