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《Contributions to Geology and Mineral Resources Research》 2012-04
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Characteristics of Sinongduo large-size overprinted and reworked Pb-Zn deposit in Xietongmen County of Tibet and the ore-searching directions

WANG Yin-chuan1,Zhou Yong2,LIU Yu-hong2,LI Rui-bao1, WEI Fang-hui1,GAO Jing-min1,LIU Cheng-jun1,WU Shu-kuan1(1.School of Earth Sciences and Resources Management,Chang'an University,Xi'an 710054,China; 2.Sichuan Province Metallurgy Geology Exploration Bureau 606 Brigade,Chengdu 611730,China)  
The Sinongduo Pb-Zn deposit is located in the Gangdese porphyry copper ore belt.Geochemistry of the granitic porphyry and dioritic porphyry shows that Sinongduo Pb-Zn deposit and the Gangdesetype porphyry deposits belong to the same metallogenic system and they were formed during and after the structure transitional period of Indian-Asia plate collision.The magma comes from the partial melting of the basement gneiss of the Precambrian Nyainqentanglha Group,which dominantly derives from greywacke and argillaceous rocks in crust,and the basaltic rocks in lower crust.Ore-forming materials originated from partial melting subduction slab of the Yarlu Zangbo Neo-Tethyan Ocean crust under the Gangdese magmatic arc and replacement of the basement of island arc by the melted materials.The formation of the ore deposit is divided into three periods.The first period was the Middle Carboniferous at which Sedex bed was formed contemporarily with carbonate rocks as the source bed.The second period was the tectonic mineralization period which was further divided into two mineralization phases.The first phase was the Late Cretaceous to the Eocene during which early hydrothermal Pb-Zn mineralization related to porphyry that may be resulted from Indian-Asia plate collision occurred.The second one is the post main Indian-Asia plate collision stretching phase at which Pb-Zn mineralization occurred and Pb,Zn from the mineralization was remobilized,overprinted and enriched due to emplacement of granitic porphyry and skarn type Pb-Zn ore bodies were formed at contact between the porphyry and the surrounding rocks and were generally controlled by complex fractures(faults).The deposits were mainly of the structural fracture zone hydrothermal fluid filling and Skarn types.The third period is mainly supergene mineralization,i.e.,dilution of the primary sulfide ore body caused by oxidation and removal of Pb,Zn oxides.The anomaly areas in south and north of the deposit are potential for further exploration.
【Fund】: 国家自然科学基金项目(编号:41172186 40972136 40572121)资助
【CateGory Index】: P618.4
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