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POLYGENETIC MINERALIZATION OF THE EARLY PROTEROZOIC TONGKUANGYU METAPORPHYRY COPPER DEPOSIT IN THE ZHONGTIAO MOUNTAINS OF CHINA
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作者 ChenW.M. ZhangC.X. +4 位作者 LuJ.R. DangZ.F. lis.p. CaiW.B. NingY.andCaoY.J. 《Geotectonica et Metallogenia》 1996年第Z1期110-111,共2页
The Tongkuangyu porphyry copper deposit in the Zhongtiao Mountains, China, is tectonically located on the southern margin of the North China platform and on the northern margin of the Late Archean Zhongtiaoshan intrac... The Tongkuangyu porphyry copper deposit in the Zhongtiao Mountains, China, is tectonically located on the southern margin of the North China platform and on the northern margin of the Late Archean Zhongtiaoshan intracontinental rift basin. The deposit occurs in a copper-bearing formation of tuffaceous variegated sandshale-K-rich bimodal volcanic rocks of the Tongkuangyu Formation of the Late Archean Jiangxian Group, and the orebodies are localized in a transition portion between tuffaceous variegated sandshale and bimodal volcanic rocks. The host rocks consist mainly of metagranodiorite-porphyry, meta-quartz monzonite- 展开更多
关键词 VOLCANIC QUARTZ MARGIN portion LOCALIZED
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