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《Journal of Jilin University(Earth Science Edition)》 2010-03
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SHRIMP U-Pb Dating of Zircon from the Fenghuangshan Quartz Monzodiorite and Granodiorite in Tongling Area,Anhui Province and Its Geological Implication

QU Hong-ying 1,2,3,PEI Rong-fu1,LI Jin-wen1,WANG Yong-lei1 1.Institute of Mineral Resources,China Academy of Geological Sciences,Beijing 100037,China 2.Graduate School,Chinese Academy of Geological Sciences,Beijing 100037,China 3.State Key Laboratory for Mineral Deposits Research,Nanjing University,Nanjing 210093,China  
In order to study the magmatic evolution and relationship between magmatism and mineralization,the SHRIMP U-Pb dating of zircon in Fenghuangshan quartz monzodiorite and granodiorite in Tongling area,Anhui Province are carried out.The SHRIMP U-Pb age of zircon from the quartz monzodiorite changes from (136.0±2.0) to (143.0±2.4) Ma,and the weighted mean age is (139.4±1.2) Ma (n=15,MSWD=0.76).Results of SHRIMP U-Pb zircon dating of granodiorite is from (136.7±2.0) to (145.3±2.4) Ma,and the weighted mean age is (141.0±1.1) Ma (n=17,MSWD=1.5).The emplacing age of the Fenghuangshan intrusion is the Late Jurassic.Moreover,the molybdenite Re-Os isochrone age is accordant with that of the granodiorite and older than the age of quartz monzodiorite.The copper mineralization has the closer relationship with the granodiorite and they are formed contemporaneously.Isotopic data indicate that the mineralization is related to the deep fluids derived from mantle magma differentiation.The extensional process resulted from the whole lithosphere thickening and the basaltic magma approaching,caused by from the aesthenosphere mantle and upper crust decompression and melting,played an important role in forming of the Fenghuangshan intrusion.
【Fund】: 中国地质调查局危机矿山项目(200799093);; 南京大学内生金属矿床成矿机制研究国家重点实验室基金项目(15-09-01)
【CateGory Index】: P597.3
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