Chronology, Geochemistry and Geological Significance of Epo Granite Intrusion, Southern Jiangxi

The Epo intrusion with an exposed area of 200 km2, is mainly composed of biotite monzonitic granite, and is located on the western margin of the Yudu-Qingtang basin, the conjunction of E-W trending Nanling tectonic-magmatic belt and the NNE trending Wuyishan tectonic belt. Situated in such a special...

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Bibliographic Details
Main Authors: GUO Na-xin, ZHAO Zheng, CHEN Zhen-yu, CHEN Yu-chuan, HOU Ke-jun, WANG Shao-yi
Format: Article
Language:English
Published: Science Press, PR China 2014-07-01
Series:Yankuang ceshi
Subjects:
Online Access:http://www.ykcs.ac.cn/cn/article/id/d75f129e-8be2-4b12-9509-c0aa83fec2ce