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《Mineral Deposits》 2009-06
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Rb-Sr and Sm-Nd isochron ages of Dongmozhazhua and Mohailaheng Pb-Zn ore deposits in Yushu area,southern Qinghai and their geological implications

TIAN ShiHong1,YANG ZhuSen1,HOU ZengQian2,LIU YingChao1,2,GAO YanGuang3,WANG ZhaoLin2,4,SONG YuCai2,XUE WanWen5,LU HaiFeng5,WANG FuChun5,SU AiNa1,6,LI ZhenZhen1,7, WANG YinXi8,ZHANG YuBao5,ZHU Tian5,YU ChangJie5 and YU YuShuai1 (1 MLR Key Laboratory of Metallogeny and Mineral Assessment,Institute of Mineral Resource,CAGS,Beijing 100037,China;2 Institute of Geology,CAGS,Beijing 100037,China;3 China Geological Survey,Beijing 100037,China;4 China Non-ferrous metals Resource Geological Survey,Beijing 100012,China;5 Qinghai Institute of Geological Survey,Xining 810012,Qinghai,China;6 East China Institute of Technology,Huzhou 344000,Jiangxi,China;7 Kunming University of Science and Technology,Kun-ming 650093,Yunnan,China;8 Center of Modern Analysis,Nanjing University,Nanjing 210093,Jiangsu,China)  
Dongmozhazhua and Mohailaheng Pb-Zn deposits in Yushu area of Qinghai Province are representative Pb-Zn deposits in the Cu-Pb-Zn polymetallic mineralization belt of the northern part of the Nujiang-Lancangjiang-Jinshajiang area,which are in the front belt of Yushu thrust nappe system.The ages of the Dongmozhazhua deposit have been determined by the Rb-Sr isochron method for sphalerite and one group of intergrowth mineral assemblage samples (pyrite and galena) and the Sm-Nd isochron method for one group of intergrowth mineral assemblage samples (sphalerite and pyrite);whereas,the ages of the Mohailaheng deposit have been determined by the Rb-Sr isochron method for sphalerite and one group of intergrowth mineral assemblage samples (sphalerite and galena) and the Sm-Nd isochron method for fluorite and one group of intergrowth mineral assemblage samples (calcite and fluorite).The ages of Dongmozhazhua and Mohailaheng deposits are 34.7~35.7 Ma with an average of 35 Ma and 31.8~33.9 Ma with an average of 33 Ma,respectively,implying they have the same mineralization epoch.Combined with geological and geochemical data,it is concluded that the Dongmozhazhua and Mohailaheng deposits formed during the same geological event and the metals have the same source.Together with regional mineralization geological setting,a possible tectonic model for metallogeny of Dongmozhazhua and Mohailaheng Pb-Zn deposits has been established.These two ages are close to the ages of the Pb-Zn deposit in Lanping basin of the southern part of the Nujiang-Lancangjiang-Jinshajiang area and in Tuotuohe basin of the northern part of the Nujiang-Lancangjiang-Jinshajiang area,indicating that it is possible that the narrow 1000 km-length belt controlled by thrust nappe system in the eastern and northern margins of Tibetan plateau would be a giant Pb-Zn mineralization belt.
【Fund】: “十一五”国家科技支撑计划重大项目(2006BAB01A08);; 国家973项目(2009CB421007);; 国土资源大调查项目(1212010818096);; 中央级公益性科研院所基本科研业务费专项资金(K0802);; 中国博士后科学基金(20070420418);; 国家基础研究计划973项目(2002GB41260);; 南京大学内生金属矿床成矿机制研究国家重点实验室资金(13-7-5);; 东华理工大学核资源与环境教育部重点实验室项目(081206)的联合资助
【CateGory Index】: P618.42
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1 ZHOU Delai1,ZHONG Kanghui1,FENG Dexin2,LI Guanqing3,GOU Jin2,HAN Wenwen1(1.College of earth Science,Chengdu University of Technology,Chengdu 610059,China;2.Tibet institute of geological survey,Lhasa 850007,China;3.Geological Survey of Tibet Autonomous Regional Geological Survey Team,Lasa 850007,China);Lead-zinc polymetallic deposits in the Tibet Autonomous Region La Nuoma geological characteristics and exploration potential analysis and then discuss[J];Sichuan Nonferrous Metals;2011-04
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