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《Acta Scientiarum Naturalium Universitatis Pekinensis》 2012-04
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Petrology and LA-ICP-MS Zircon U-Pb Geochronology of the Qianjinchang Pluton,Southeastern Inner Mongolia

XU Jiajia1,2,LAI Yong1,,CUI Dong3,LU Bin3 1.The Key Laboratory of Orogenic Belts and Crustal Evolution(MOE),School of Earth and Space Sciences,Peking University,Beijing 100871;2.China Geological Library,Beijing 100083;3.No.10 Institute of Geological Exploration,Inner Mongolia Bureau of Geology and Mineral Resources,Chifeng 024005  
The Qianjinchang biotite granite from southeastern Inner Mongolia is located in the suture zone between the Siberian and North China Cratons.The Daolundaba Cu-W-Sn polymetallic deposit formed at the contact zone between the north-west margin of the pluton and the Lower Permian Linxi Formation.The biotite granite is high-K calc-alkaline and peraluminous,with Na2O+K2O: 6.12% to 9.31%,Al2O3: 14.42% to 15.59%,A/CNK: 1.09 to 1.22,and a mean δ value of 2.41.The rock samples lie within the S-type granite region in the ACF plot.They are depleted in Sr(89.91 to 192.80 μg/g),Ba,Eu(δ Eu: 0.46 to 0.81) and ∑REE(102.65 to 237.92 μg/g),but slightly enriched in Yb(2.17 to 3.46 μg/g) and La,consistent with the characteristics of S-type granites.The rocks further fall in the region of post-collisional granite in the Rb vs.Y+Nb diagram.LA-ICP-MS zircon U-Pb geochronology shows that the pluton emplaced at(273 ± 7.7) to(278 ± 4.3) Ma.These Permian granite rocks probably formed in an extensional setting that postdated the collision between the Siberian and North China Cratons.
【Fund】: 中国地质调查局地质调查工作项目(1212010813045)资助
【CateGory Index】: P597.3
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