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《Earth Science(Journal of China University of Geosciences)》 2009-01
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U-Pb Ages of Detrital Zircon from Meta-Sedimentary Rock from the Huwan Shear Zone,Western Dabie Terrain and Their Geological Significance

YANG Sai-hong1,WU Yuan-bao1,2,LIU Xiao-chi1,WANG Jing1,PENG Min1,JIAO Wen-fang11.State Key Laboratory of Geological Processes and Mineral Resources,Faculty of Earth Sciences,China University of Geosciences,Wuhan430074,China2.MOE Key Laboratory of Continental Dynamics,Department of Geology,Northwest University,Xi'an710069,China  
The Huwan high-pressure(HP)metamorphic zone is a key region to investigate the evolution process and timing of the Qinling-Dabieshan-Sulu orogenic belt.However,the timing of eclogite-facies metamorphism in this zone has not been well constrained.In order to constrain the time of eclogite-facies metamorphism,zircons from a metasediment sample HXD98-9 near Xiongdian were selected for LA-ICPMS U-Pb dating and trace element analysis.Metamorphic zircons are characterized by weak or none zoning,low Th/U ratios,low and/or flat HREE patterns,and an insignificantly negative Eu anomaly.These reflect that the metamorphc zircons crystallized with the presence of garnet and the absence of plagioclase feldspar,which occurred in eclogite-facies conditions.The weighted mean 206Pb/238U age of 310±3Ma for these metamorphic zircons is thus the best estimated age of the eclogite-facies metamorphism in this HP metamorphic zone.Three groups of U-Pb age were obtained from the inherited magmatic zircons,ranging of(400±5Ma)-(419± 5Ma),(426±5Ma)-(449±5Ma),and(496±5Ma)-(524±7Ma),respectively.One inherited grain has a U-Pb age of 580.7±7.3Ma.These indicate that the inherited zircons were mostly derived from southern part of the North China block,while some from the Yangtze block.
【Fund】: 国家自然科学基金项目(Nos.40873043 90714010 40772042);; 教育部项目(Nos.IRT0441 B07039 NCET-06-0659);; 西北大学大陆动力学重点实验室基金
【CateGory Index】: P597.3
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