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《Acta Sedimentologica Sinica》 2006-03
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The Origin of Sandstones from the Songpan-Ganze Basin,Sichuan,China: evidence from SHRIMP U-Pb dating of clastic zircons

LAN Zhong-wu~(1,2) CHEN Yue-long~(1) SU Ben-xun~(1,2) LIU Fei~(1) ZHANG Hong-fei~(3)(1.College of Earth Sciences and Resources,Chinese University of Geosciences,Beijing 100083;2.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029;3.Graduate School,Chinese Academy of sciences,Beijing 100049;4.School of Earth Sciences,Chinese University of Geosciences,Wuhan 430074)  
The Songpan-Ganze basin(Central China) covers a huge triangular area of more than 200,000km~(2)and is bounded by the continental blocks of South China,North China and the Tibetan plateau.The six sandstone samples collected from this belt were analyzed grain-by-grainusing SHRIMP U-Pb method.The detrital zircons yield a wide range of ages,whichare focused on Proterozoic with minor contribution from late Archean material.The discordance and Pb loss patterns from low U zircons indicate that they might be resulted from the subsequent magmatism events,including the Sibao to the Indosinian periods.The Caledonian appearance of zircons indicates that the origin of these clastic sediments might originate from the Northern Qinling belt,other zircons originated mainly from the north margin of the Yangtze craton and the south Qinling belt.
【Fund】: 国家自然科学基金(批准号:40234052);; 教育部重点科研项目(重点03032)共同资助
【CateGory Index】: P588.212.3
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9 JIANG Zi-qi1,2,WANG Qiang1,WYMAN D.A.3,TANG Gong-jian1,2,JIA Xiao-hui1,YANG Yue-heng4 and YU Heng-xiang5 1.State Key Laboratory of Isotope Geochemistry,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640,China;2.Graduate University of Chinese Academy of Sciences,Beijing 100049,China;3.Division of Geology and Geophysics,School of Geosciences,the University of Sydney,NSW 2006,Australia;4.State Key Laboratory of Lithosphere Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;5.Department of Resource Exploration Engineering,School of Geosciences,Guilin University of Technology,Guilin 541004,China;Origin of ~30 Ma Chongmuda adakitic intrusive rocks in the southern Gangdese region,southern Tibet:Partial melting of the northward subducted Indian continent crust?[J];Geochimica;2011-02
10 LI Xiang-hui 1 ,WANG Cheng-shan2,LIU Shu-gen3,RAN Bo3,XU Wen-li 3,ZHOU Yong3,ZHANG Zhi-jing3 1.State Key Laboratory of Mineral Deposit Research,School of Earth Sciences and Engineering,NanjingU niversity,Nanjing 210093,China 2.School of the Earth Sciences and Resources,China University of Geosciences,Beijing 100083,China 3.State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,ChengduU niversity of Technology,Chengdu 610059,China 4.The 402th Geological Survey,Sichuan Bureau of Geology and Mineral Resources,Chengdu 611730,China;Lithofacies of the Upper Middle Triassic Guanggaishan Formation in Both Sides of the Bailongjiang Uplift,Southwestern Qinling Orogenic Belt:Implications to the Basin Analysis[J];Earth Science(Journal of China University of Geosciences);2012-04
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1 Jun Gao~(a*).Reiner Klemd~b,Qing Qian~a,Xi Zhang~a,Jilei Li~(a,b),Tuo Jiang~a,Yongqiang Yang~c ~aKey Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,P.O.Box 9825,Beijing 100029,China ~bGeoZentrum Nordbayern,Universitt Erlangen,Schlossgarten 5a,91054 Erlangen,Germany ~cState Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Beijing 100083,China;The collision between the Yili and Tarim blocks of the Southwestern Altaids:Geochemical and age constraints of a leucogranite dike crosscutting the HP-LT metamorphic belt in the Chinese Tianshan Orogen[A];[C];2012
2 HUANG Bao-Chun,CHEN Jun-Shan,YI Zhi-Yu State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics, Chinese Academy of Sciences,Beijing 100029,China;Paleomagnetic discussion of when and where India and Asia initially collided[A];[C];2011
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4 Wei-Qiang Ji~(a,*),Fu-Yuan Wu~a,Chuan-Zhou Liu~a,Sun-Lin Chung~b a State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,P.O.Box 9825,Beijing 100029,China b Department of Geosciences,National Taiwan University,Taipei 106,Taiwan;Early Eocene crustal thickening in southern Tibet:New age and geochemical constraints from the Gangdese batholith[A];[C];2013
5 Junxing ZHAO,~(1,2) Kezhang QIN,~1 Guangming LI,~1 Jinxiang LI,~1 Bo XIAO~(1,2) and Lei CHEN~(1,2) 1 Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences and 2 Graduate University of Chinese Academy of Sciences,Beijing,China;Geochemistry and Petrogenesis of Granitoids at Sharang Eocene Porphyry Mo Deposit in the Main-Stage of India-Asia Continental Collision,Northern Gangdese,Tibet[A];[C];2013
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