Crustal development of the Hida belt, Japan: Evidence from Nd–Sr isotopic and chemical characteristics of igneous and metamorphic rocks-Reference-Cited by-同舟云学术

Crustal development of the Hida belt, Japan: Evidence from Nd–Sr isotopic and chemical characteristics of igneous and metamorphic rocks

Published:2000-12 Issue:1-2 Volume:328 Page:183-204
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Arakawa Yoji,Saito Yutaka,Amakawa Hiroshi

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference85 articles.

1. Re-examination of Pre-Cretaceous basement rocks in Korea by CHIME geochronology;Adachi;J. Geography,1995

2. 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

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

4. Two types of granitic intrusions in the Hida belt, Japan: Sr isotopic and chemical characteristics of the Mesozoic Funatsu granitic rocks;Arakawa;Chem. Geol.,1990

5. Strontium isotopic compositions of Mesozoic granitic rocks in the Hida belt, central Japan: diversities of magma sources and processes of magma evolution in a continental margin area;Arakawa;Lihtos,1990

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