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《Geochimica》 2008-05
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SHRIMP U-Pb zircon geochronology and geochemistry of the Guandian pluton in central Anhui,China:Petrogenesis and geodynamic implications

ZIFeng1,2,W ANG Qiang1,TANG Gong-jian1,2,SONG Biao3,XIE Lie-wen4,YANG Yue-heng4,LIANG Xi-rong1,TU Xiang-lin1and LIU Ying1 1.Key Laboratory of Isotope Geochronology and Geochem istry,Guangzhou Institute of Geochem istry,Chinese Academ y of Sciences,Guangzhou 510640,China;2.Graduate University ofChinese Academ y ofSciences,Beijing 100049,China;3.Institute ofGeology,Chinese Academ y ofGeologicalSciences,Beijing 100037,China 4.Institute ofGeology and Geophysics,Chinese Academ y ofSciences,Beijing 100029,China  
The Guandian pluton,which is located in the eastern Yangtze block,occurs along the southern segm ent of Tan-Lu fault belt.It m ainly consists of quartz m onzonite and m onzonite.New zircon SH RIM P U-Pb age data suggestthatitintruded in(131.5±1.6)M a.The rocks ofthis pluton are interm ediate-felsic(SiO254.84% ~ 67.83%)and high-K calc-alkaline.They are geochem ically characterized by relatively high Al2O3(14.12% ~ 15.14%),Sr(612~976μg /g)and Sr/Y(31~77),La /Yb(18~42)values,butlow Y(8.20~21.4μg /g)and Yb(0.90~1.70μg /g)contents with negligible to positive Eu anom alies(δEu 0.73~1.58),sim ilar to adakites.The Guandian intrusive rocks exhibithom ogeneous initial87Sr/86Sr ratios(0.7058~0.7061)butlow εNd(t)values(-17.03~-15.11),as well as relatively hom ogeneous and low zircon εHf(t)(-26.3~-22.6),indicating thatthey were im possibly derived by partialm elting ofsubducting oceanic crust.They also have relatively high M gO(2.21% ~6.75%),M g#(56~62)and com patible elem ents(Cr85.4~356μg /g,Ni 40.8~144 μg /g),suggesting that they should contain som e m antle com ponents.Taking into account geochronologic,geochem ical,Sr-Nd and zircon H fisotopic data,we suggestthe Guandian adakitic m agm as were m ostlikely derived by partialm elting ofdelam inated lowercrust,and laterly contam inated atdifferentpercentage by m antle peridotites.In Early Cretaceous,the activities ofthe Tan-Lu faultand the crustaldetachm entofeastern Yangtze block after the collision between Yangtze and North China blocks possibly resulted in lower crustal delam ination and associated adakitic m agm atism.
【Fund】: 中国科学院知识创新工程重要方向项目(KZCX2-YW-128);; 国家自然科学基金(40572042 40673037)
【CateGory Index】: P597
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