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《Journal of Jilin University(Earth Science Edition)》 2008-01
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A Further Discussion of the Petrogenesis and Tectonic Implication of the Mazhashan Syenites in the Bachu Area

SUN Lin-hua1,2,WANG Yue-jun1,FAN Wei-ming1,ZI Jian-wei11.Key Laboratory of Isotope Geochronology and Geochemistry,Guangzhou Institute of Geochemistry, Chinese Academy of Sciences,Guangzhou 510640,China2.Graduate University,Chinese Academy of Sciences,Beijing 100039,China  
The Mazhashan syenites in the Bachu area were formed in the Late Permian with the zircon SHRIMP age ranging from 286 to 277Ma,and these ages are consistent with the ages(300-260 Ma) of the post-collisional granites in the southern Tianshan orogen.These syenites are high in silica and alkaline with SiO2=62.98%-67.29 % and K2O+Na2O=10.08%-11.22 %,and often show Na2OK2O.Most of the samples have positive Eu anomalies and slightly negative Sr and significantly negative P and Ti anomalies.They formed in an intra-plate rifting setting as they have geochemical affinity with A1-type granites with Ga/Al =(2.84-3.28)×10-4 and Zr+Nb+Ce+Y =(405.11-606.49)×10-6.The syenites have more depleted Sr-Nd isotopic compositions(εNd(t) =+3.4-+4.3,ISr=0.703 03-0.703 44) and younger Nd model ages(TDM=0.6-0.7 Ga) than the coeval mafic dikes.Geochemical data indicate that the syenites were originated from the remelting of the underplated mafic lower crust which composition had been changed by the asthenospheric upwelling.Combining with regional geological data,the authors found that the magmatic activity differences between the Tarim Basin and the South Tianshan Orogen in the Permian stage were probably related to their different tectonic localities.The Permian magmatism in the Tarim Basin was related to the active rifting triggered by the asthenospheric upwelling,this is different from the magmatism during the post-collisional extension in the South Tianshan Orogen,which was controlled by the pre-existent mobile zone(suture) or by the extension-resulted detachment zones.
【Fund】: 国家自然科学基金项目(40421303 40304039);; 中国科学院知识创新项目(KZCX2-YW-128)
【CateGory Index】: P588.122
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4 Zhou Jiulong1,Luo Zhaohua1,*,He Huaiyu2,Sun Jing31.State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Beijing100083,China2.Key Laboratory of the Earth's Deep Interior,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing100029,China3.The No.4 Team of the Bureau of Geology and Exploration of Hebei Province,Chengde 067000,China;New~(40)Ar/~(39)Ar geochronologic constraint on the age of Damiao Fe-Ti-P deposits,North China Craton and its geological significance[J];Earth Science Frontiers;2012-04
5 ZHOU Zuomin,XIE Caifu,XU Qian,GAO DafeiKey Laboratory of Fundamental Science on Radioactive Geology and Exploration Technology;Key Laboratory of Nuclear Resources and Environment,Ministry of Education;School of Earth Sciences,East China Institute of Technology,Fuzhou,Jiangxi Province,344000;Geological and Geochemical Characteristics of Middle Triassic Syenite—Granite Suite in Hainan Island and Its Geotectonic Implications[J];Geological Review;2011-04
6 HUANG He1),ZHANG Zhaochong1),ZHANG Dongyang1),DU Hongxing2),MA Letian3),KANG Jianli1),XUE Chunji1)1) China University of Geosciences,State Key Laboratory of Geological Processes and Mineral Resources,Beijing,100083;2) Xinjiang Bureau of Geology and Mineral Resources,Urumqi,830000;3) School of Earth and Space Sciences,Peking University,Beijing,100871;Petrogenesis of Late Carboniferous to Early Permian Granitoid Plutons in the Chinese South Tianshan: Implications for Crustal Accretion[J];Acta Geologica Sinica;2011-08
7 QIAO Wen-lang1,XIAO Jia-fei2,CHEN Wu1,YAO Yi-xiang1(1.Guizhou Academy of Geologic Survey,Guiyang 550005,Guizhou,China;2.State Key Laboratory of Ore Deposit Geochemistry Chinese Academy of Sciences,Guiyang 550002,Guizhou,China);Geochemical Characteristic and Structural Environment of Intrusive Rock in Yiwu Area of East Tianshan Mountain[J];Guizhou Geology;2011-04
8 LI Jie 1,2),CHEN Wen 1),YONG Yong 1),CHEN Yue-long 2),SUN Jing-bo 1),ZHANG Yan 1),LIU Xin-yu 1),YANG Li 1) 1) National Key Laboratory of Continental Structure and Dynamics,Laboratory of Isotope Thermochronology,Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037;2) China University of Geosciences,Beijing 100083;Emplacement Age,Geochemical Characteristics and Tectonic Significance of Zhaxike Quartz Diorite in Yushu Area,Qinghai Province[J];Acta Geoscientica Sinica;2012-05
9 WANG Qiang1,SUN Yan1,ZHANG Xue-hui2,ZHANG Shi-ming1,WANG Yu-liang1,ZHANG Chun-mao1(1.Chengdu University of Technology,Chengdu 610059,Sichuan,China;2.Nanjing Institute of Geology and Mineral Resources,Nanjing 210016,Jiangsu,China);Zircon LA-ICP-MS U-Pb age of plagiogranite porphyry in the Cunqian copper polymetallic deposit of Jiangxi Province and its geological implications[J];Geology in China;2012-05
10 LIU Chun-hua1,LEI Min1,WU Cai-lai1,YIN Jing-wu2,SHAO Xing-kun3,YANG Hai-tao4(1.Institute of Geology,CAGS,Beijing 100037;2.Chinese University of Geosciences,Beijing 100083;3.Detachment of General Gold Party,Chinese People’s Armed Police Force,Mudanjiang Heilongjiang 157021;4.North-west institute of nonferrous metals geology,Xi’an Shaanxi 710054,China);Backscattered electron detection and the charactetistics of cathodoluminescence of the minerals in A-type granitoids from Boziguoer,Baicheng County,Xinjiang[J];Journal of Chinese Electron Microscopy Society;2013-01
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1 LIU Xin,QIAN Qing,SU Wen and LI JiLei 1.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.Graduate University of Chinese Academy of Sciences,Beijing 100049,China 3.Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 4.GeoZentrum Nordbayern,Universitt Erlangen,Schlossgarten 5a,91054 Erlangen,Germany;Pluton from Muhanbasitao in the western of Awulale,Western Tianshan:Geochemistry,geochronology and geological implications[A];[C];2013
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