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《Journal of Jilin University(Earth Science Edition)》 2012-S1
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Geochemical Characteristics of Late Paleozoic-Early Mesozoic Bayinsukhtu Monzonitic Granite and It's Constraints on Tectonic Setting in Southeastern Mongolia

Shen Xiao-li1,2,Zhang Bao-lin1,Jia Wen-chen1,Guo Zhi-hua1,2,Huang Xue-fei1,2,Cui Min-li1 1.Key laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.Graduate University of Chinese Academy of Sciences,Beijing 100049,China  
Located between the northern margin of Erlian-Hegenshan suture zone and the pericontinental accretion zone of the southeastern margin of the Siberia plate,the Bayinsukhtu granitic body is an intrusive complex composed of monzonitic granites emplaced at Carboniferous and Triassic-Jurassic respectively.Geochemical analyses suggest that both of the two periods of monzonitic granites are characterized by high contents of silica,Al2O3 and alkali,low contents of calcium and magnesium.They are enriched in LILE and depleted in HFSE,with moderately enrichment of LREE,weak fractionation of LREE from HREE and negative Eu anomalies(δEu = 0.35-0.66).Based on the petrologic and geochemical features,the Carboniferous monzonitic granite is classified as mainly high-K,calc-alkaline,metaluminous to weakly peraluminous syn-orogenic I-type granite,while the latter is A-type granite.Isotope geochemistry of the Carboniferous granite shows that values of εNd(t) and(87Sr/86Sr)i range from 0.9 to 1.5,and from 0.700 62 to 0.704 82,respectively,which indicates that the granitic magma was likely derived from a young mantle source or an accretionary island arc with some degree of crustal contamination.However,the Triassic-Jurassic granite has lower εNd(t) but higher(87Sr/86Sr)i values relative to the Carboniferous granite,ranging from-0.3 to 0.3 and from 0.709 96 to 0.710 19,respectively.This indicates the granite derived from the same source with relatively high degree of crustal contamination.The dating of zircons from the monzonitic granites determined by LA-ICP-MS yielded a weighted age of(296±3.5) Ma,indicating that in the late Carboniferous the studied area was a syn-collision pericontinental tectonic environment.According to geochemical analysis of Late Triassic-Early Jurassic granite,it is presumed that the syn-collisional magmatism lasted till Triassic-Jurassic,probably suggestive of a long duration of collision.
【Fund】: “十一·五”科技支撑计划重大项目(2006BAB01A02)
【CateGory Index】: P588.121
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