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《Chinese Geology》 2004-02
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SHRIMP U-Pb geochronology of the Xinqiao Cu-S-Fe-Au deposit in the Tongling ore district, Anhui

WANG Yan-bin1, Liu Dunyi1, MENG Yi-feng2, ZENG Pu-sheng2, YANG Zhu-sen2, TIAN Shi-hong2(1. Beijing SHRIMP Lab, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China;2. Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China)  
High-precision SHRIMP U-Pb dating was performed on zircon from quartz diorite and diabase in the Xinqiao Cu-S-Fe-Au deposit, Tongling ore district, Anhui. Zircon from quartz diorite yielded a 206Pb/238U age of (140.4±2.2) Ma, while the zircon age of diabase is relatively complex. Several Proterozoic zircon grains were found in diabase, which yielded 207Pb/206Pb ages of (2 261±14) Ma, (1 612±8) Ma, (919±12) Ma and (831±17) Ma. In addition, there is also a group of Early Paleozoic zircon grains, whose 206Pb/238U age is (443±13) Ma. The above new data give the information of the possible existence of Proterozoic basement in this district, and Yanshanian magmatism is of great significance for mineralization in the district.
【Fund】: 国土资源部国际合作与科技司重点项目(20010209);; 中国地质调查局地质大调查项目(200110000004);; 国土资源部专项(20010103)资助。
【CateGory Index】: P618.41
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