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《Geochimica》 2004-06
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Metallogenic epoch of Zhulazaga gold deposit in Alxa area,Inner Mongolia Autonomous Region

LI Jun-jian 1,2 ,LUO Hui 2 ,ZHOU Hong-ying 1,2 ,SANG Hai-qing 3 ,QIN Zhi-an 2 ,WANG Shou-guang 4 ,SUN Zheng-ping 4 1.School of Earth Sciences and Resourc es,China University of Geosciences,Beijing100083,China;2.Tianjin Institute of Geology and Min eral Resources,China Geological Survey,Tianjin300170,China;3.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beiji ng100029,China;4.Inner Mongolia Geological Survey,H ohhot010020,China Correspondence should be addressed to LI Jun-jian(E-mail:tjljunjian@cgs.gov.cn)Received September 27,2003;revised April 8,2004;accepted July 19,2004;published November,2004  
Zhulazaga gold deposit is a supper la rge stratabound-reconstructive gold ore deposit that has been found in recent years in Alxa area,Inner Mo ngolia Autonomous Region.The gold d eposit occurs in Mesoproterozoic strata and is of great ore potential.The host rocks are mainly calcareous siltstone and silty slate.Single zircon U-Pb and quartz 40 Ar / 39 Ar methods are applied to determination of U-Pb ages of metallogenic periods granite-porphyry and postmetallogenic periods diorite-porphyrite,and 40 Ar / 39 Ar age of Au-bearing quartz-sulfide ore body.The results show formation ages of(304±5)Ma of the zircon from the granite-porphyry and(259±6)Ma from the diorite-porphyrite.The quartz fro m the Au-bearing quartz-sulfide ore body shows a plateau age of(282.3±0.9)Ma.The Rb-Sr age of Au-bearing sulfi de ore measured before was(275±6)Ma.The close coincidence indicates that Zhulazaga gold deposit was form ed in late Variscan.The gold deposit,together with the other late Varisc an gold deposit,such as Hulunxibai gold dep osit and Oubulage copper-gold deposit in Alxa area,imply that Variscan i s the major Au(Cu)ore-forming epoch in West China.
【Fund】: 中国地质调查局国土资源大调查项目(19991020218003200110200038);; 科学技术部社会公益研究专项资金项目(2001DIB10056)
【CateGory Index】: P618.51
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