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《Acta Mineralogica Sinica》 2005-01
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DETERMINATION OF ORE- AND ROCK- FORMING TIME OF THE MACHANGQING PORPHYRY Cu(Mo) DEPOSIT, WESTERN YUNNAN PROVINCE

PENG Jian-tang~(1),BI Xian-wu~(1),HU Rui-zhong~(1), WU Kai-xing~(1),SANG Hai-qing~(2)(1.Institutte of Geochemistry, Chinese Academy of Sciences; Guiyang 550002, China; 2. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China)  
The alkali-rich intrusive rocks at Machangqing, western Yunnan Province are a composite rock massif which is characterized by multi-episodic magmatic intrusion. The earliest magma intrusive activities started at 52 Ma; the medium ones at 42-47 Ma; the late ones were most intense at 33-37 Ma; and the final-stage magmatic activities started at 29-32 Ma. The early metallogenesis of the Machangqing Cu-Mo deposit occurred at about 37-40 Ma, while the late metallogenesis occurred at about 34-35 Ma, just in consistency with the forming time of other ore deposits regionally associated with the alkali-rich intrusive rocks. The Machangqing Cu-Mo deposit is closely associated both in time and in space with the alkali-rich intrusive rocks, and its metallogenesis is related mainly to the late-stage magma intrusive activities.
【Fund】: 中科院"西部之光"项目;; 中国科学院知识创新项目(KZCX2 101)
【CateGory Index】: P618.41
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