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《Geology in China》 2010-01
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Zircon U-Pb chronologic evidence for magma mixing in the Weiya ore district,Xinjiang

LI Mei1,WANG Yu-wang1,WANG Jing-bin2,WANG Li-juan2,LONG Ling-li2(1.Department of Geography,Xinzhou Normal University,Xinzhou 034000,China;2.Beijing Institute of Geology for Mineral Resources,Beijing 100012,China)  
Lithological,mineral chemical and lithogeochemical characteristics of K-feldspar granite in the Weiya V-Ti-magnetite ore district in eastern Xinjiang as well as the enclaves(diorite) and field geological features of this granite suggest a product of magma mixing.This paper obtained zircon U-Pb ages of(247.5±5.3) Ma and(244.8±1.8) Ma from the K-feldspar granite and its mafic microgranular enclaves of diorite,which are in accord with the age of(244.7±3.3) Ma from the quartz monzodiorite within the error limits.The dating result provides the evidence for magma mixing origin of K-feldspar granite and its enclaves from the viewpoint of chronology.
【Fund】: 国家重点基础研究发展规划项目(2007CB411304和2001CB409806)资助
【CateGory Index】: P588.125
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