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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2007-04
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Characteristics and metallogenic model of the Pulang superlarge porphyry copper deposit in Yunnan,China

LI Wen-chang1,ZENG Pu-sheng21.Faculty of Earth Sciences and Resources,China University of Geosciences,Beijing 100083,China;2.Department of Resources and Environment,Yunnan University of Finance and Economics,Kunming 650021,China  
The westward subduction of the Ganze-Litang Paleo-ocean occurred earliest in the late Early Triassic,and up to the Late Triassic,the plate of the Ganze-Litang Paleo-ocean subducted in a large-scale beneath the Zhongza massif to lead to the formation of the Yidun island arc belt(YIAB).The Pulang porphyry copper deposit is just located at the southern end of YIAB,and is regarded as the typical Triassic porphyry copper deposit in China up to now.The deposit is hosted in a composite intrusion in the form of a stock consisting of quartz diorite porphyry and quartz monzonite porphyry.The host intrusion is quartz monzonite porphyry occupying an area of 1.09 km2.By Re-Os dating for molybdenite and K/Ar,Ar/Ar dating for thermal minerals,such as biotite and orthoclase,and whole rock from the Pulang porphyry copper deposit,the mineralization period of the porphyry copper deposit is determined for the first time.The duration of thermal activity involving patassic silicates(biotite and K-feldspar) alteration ranges from(235.4±2.4) Ma to(221.5±2.0) Ma determined by K-Ar dating.The age of the quartz-molybdenite stage is (~213±3.8) Ma by molybdenite Re-Os dating,the plateau ages(214.58±0.91) Ma to(216.0±1) Ma of the biotite from the main Cu-bearing orebody and Cu-Mo-bearing orebody of the Pulang district are the Late Triassic Norian,consistent with the Re-Os dating.These data suggest that the ore-formation of the Pulang porphyry copper deposit developed in Indosinian.The host intrusion has a distinct alteration zoning from the centre outward,formed the strong silisification zone(locally) →potassic silicate(K-felspar + biotite) zone→phyllic zone→propyllic zone(locally developed illite-carbonate zone).The industrial orebodies are mainly hosted within the zones of potassic silicate and phyllic of the quartz monzonite porphyry.The deposit is of the three-storeyed model which consists of the orebodies with structures of dissaminated at the lower part,veinlet-stockwork at the middle-upper part,and the vein or lode at the top.Up to now,the proved copper resources of the deposit is up to the superlarge scale of copper deposit.The characteristics of the intrusion,element assemblage,and mineralization of the deposit can be compared with the Oyu Tolgoi porphyry copper deposit in Mongolia.
【Fund】: 国家自然科学基金资助项目(40272046);; 中国地质调查局资助项目(200110200009);; 国土资源大调查项目(20021020001)
【CateGory Index】: P618.41
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