New SHRIMP U-Pb zircon ages of granitic rocks in the Hida Belt, Japan: Implications for tectonic correlation with Jiamushi massif-Reference-Cited by-同舟云学术

New SHRIMP U-Pb zircon ages of granitic rocks in the Hida Belt, Japan: Implications for tectonic correlation with Jiamushi massif

Published:2013-09-11 Issue:4 Volume:22 Page:508-521
ISSN:1038-4871
Container-title:Island Arc
language:en
Short-container-title:Island Arc

Author:

Zhao Xilin¹,Mao Jianren¹,Ye Haimin¹,Liu Kai¹,Takahashi Yutaka²

Affiliation:

1. Nangjing Institute of Geology and Mineral Resources; Nanjing 210016 China

2. Institute of Geology and Geoinformation Center; Geological Survey of Japan; AIST; Tsukuba 305-8567 Japan

Publisher

Wiley

Subject

Geology

Reference71 articles.

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2. Two contrasting types of Rb-Sr isotope systems for the Funatsu granitic rocks in the northwestern part of the Hida belt, central Japan;Arakawa;Journal of the Japanese Association of Mineralogists, Petrologists, and Economic Geologists,1988

3. 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;Arakawa;Lithos,1989

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

5. Crustal development of the Hida belt, Japan: Evidence from Nd-Sr Isotopic and chemical characteristics of igneous and metamorphic rocks;Arakawa;Tectonophysics,2000

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