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...
| Main Authors: | , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Science Press, PR China
2014-07-01
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| Series: | Yankuang ceshi |
| Subjects: | |
| Online Access: | http://www.ykcs.ac.cn/en/article/id/d75f129e-8be2-4b12-9509-c0aa83fec2ce |