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《Geological Review》 2006-03
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SHRIMP Zircon U-Pb Dating of the Intrusive Rocks in the Dachang Tin—Polymetallic Ore Field, Guangxi and Their Geological Significance

CAI Minghai 1) , HE Longqing 2) , LIU Guoqing 2) , WU Decheng 3) , HUANG Huimin 3) 1) College of Resource and Environment, Guangxi University, Nanning, Guangxi, 530004 2) Yichang Institute of Geology and Mineral Resources, Geological Survey of China, 443003 3) Liuzhou Huaxi Co.Ltd., Liuzhou, Guangxi, 545006  
The SHRIMP zircon U-Pb method was used to determine the ages of magmatites of the Dachang tin—polymetallic ore field. The Longxianggai biotite granite, which is the main part of the Longxianggai granite stock, was dated at 93±1 Ma (2σ, 8 spots, MSWD=1.6), porphyritic granite at 91±1 Ma (2σ, 10 spots, MSWD=1.7), granite-porphyry dyke (Eastern Dyke) at 91±1Ma (2σ, 12 spots, MSWD=1.13) ,and quartz dioritic porphyrite (Western Dike) at 91±1 Ma (2σ, 8 spots, MSWD=1.11). These data indicate that intrusive rocks in the Dachang tin district occurred in Middle Cretaceous, and that the mineralization and magmatic emplacement took place simultaneously and resulted from the same tectono-thermal event.
【Fund】: 柳州华锡集团有限责任公司博士后工作站科研项目“丹池成矿带构造控矿规律研究”资助成果。
【CateGory Index】: P618.44
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