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《EARTH SCIENCE FRONTIERS》 1999-04
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FORMATION AND TECTONIC BACKGROUND OF THE NORTHERN QILIAN OROGENIC BELT

Ge Xiaohong Liu Junlai(Dept.Earth Sci.,Changchun Univ.Sci.Tech.,Changchun,130026)  
The northern Qilian orogenic belt is an intraplate orogenic belt formed on the basis of the Neoproterozoic craton.Three stages of tectonic evolution of the belt are recognized:(1)An oceanic trough,instead of an oceanic Basin was formed in the early Palaeozoic due to the break down of the craton.The western extension of the trough,corresponding to the Manjia'er Awati depression to the north of the Tarim Basin, is sinistrally displaced by the Altun fault zone for about 340 km, and they constitute one entire aulacogen in the early Palaeozoic.The “Qilian event” led to the closing of the aulacogen in late early Paleaozoic;(2) Planation of the Paleao Qilian Mountains and consequent stable sedimentation as a part of cratonic basin dominated in the late Palaeozoic Mid Triassic.The collision of the Qiangtang Plate at the end of the Mid Trassic resulted in the Indosinian intraplate folding,however,without the occurrence of orogenic belt;(3) From Mesozoic to Tertiary is a stage of peneplanation in North Qilian Mountains and the orogenic belt was finally formed as a result of nappe thrusting type mountain building process during the Late Himalayan tectonic movement at the latest Early Pleistocene,which is compatible with the uplifting of the Tibet Plateau.Both processes were controlled by the continent continent collision of the Indian Plate with the Eurasia Plates.
【Fund】: 国家自然科学基金项目
【CateGory Index】: P542
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10 XIAO Gen-ru1,2,GAN Wei-jun1,CHEN Wei-tao1,CHENG Jia3 1.Institute of Geology/State Key Laboratory of Earthquake Dynamics,China Earthquake Administration,Beijing 100029,China 2.School of Surveying and Mapping,East China Institute of Technology,Fuzhou,Jiangxi 344000,China3.China Earthquake Network Center,Beijing 100045,China;Present-Day Movement of Bangong Co-Nujiang Suture Zone,Tibetan Plateau,Inferred from GPS Measurements[J];Journal of Jilin University(Earth Science Edition);2010-06
China Proceedings of conference Full-text Database 10 Hits
1 QIU Zhen,WANG QingChen and YAN DeTian 1.State Key Laboratory of Lithospheric Evolution,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 Tectonics and Petroleum Resources of Ministry of Education,University of Geosciences,Wuhan 430074,China;Geochemistry and sedimentary background of the Middle-Upper Permian cherts in the Penglaitan section,Laibin,Guangxi Province[A];[C];2012
2 ZHAN Tao~(1,2),GUO ZhengTang~(1*),WU HaiBin~1,GE JunYi~1,ZHOU Xin~1, WU ChunLin~(1,2) & ZENG FangMing~(1,2) 1 Key Laboratory of Cenozoic Geology and Environment,Institute of Geology and Geophysics, Chinese Academy of Sciences,Beijing 100029,China; 2 Graduate University of Chinese Academy of Sciences,Beijing 100049,China;Thick Miocene eolian deposits on the Huajialing Mountains:The geomorphic evolution of the western Loess Plateau[A];[C];2012
3 ZHANG Qi (Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China);GUESS ON THE SILURIAN-DEVONIAN NORTH CHINA HIGHLAND:EVIDENCE FROM THE INFORMATION OF GANSU[A];[C];2012
4 Gao Zhiyong~(1,2) Zhang Shuichang~(1,2) Li Jianjun~3 Zhang Baomin~(1,2) Gu Qiaoyuan~3 Lu Yuhong~3 1 Petroleum Geology Research and Laboratory Center,Research Institute of Petroleum Exploration & Development,Petro China,Beijing 100083 2 State Key Laboratory of Enhanced Oil Recovery,Research Institute of Petroleum Exploration and Development,Petro China,Beijing 100083 3 Research Institute of Petroleum Exploration and Development, Tarim Oilfield Corporation,Petro China,Korle 841000,Xinjiang;Distribution and sedimentary environments of Salgan and Yingan shales of the Middle-Upper Ordovician in western Tarim Basin[A];[C];2010
5 Chen Ling,Zhu Rixiang,Wang Tao Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;Progress in continental lithosphere studies[A];[C];2008
6 Yuan Baoyin~①Guo Zhengtang~①Hao Qingzhen~①Peng Shuzhen~(①②) Qiao Yansong~③Wu Haibin~④Xiao Guoqiao~(④⑤) Ge Junyi~(④⑤) Sun Bin~(①⑤) Zhou Xin~(④⑤) Yin Qiuzhen~(①⑤) Liang Meiyan~(①⑤)Qin Li~(①⑤) Liu Lian~(①⑤) Yao Zhengquan~(④⑤) Liu Tungsheng~①(①Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029;②Taishan College,Tai'an 271021;③Institute of Geomechanics,Chinese Academy of Geological Sciences,Beijing 100081;④Institute of Earth Environment,Chinese Academy of Sciences,Xi'an 710075;⑤Graduate University of Chinese Academy of Sciences,Beijing 100049);CENOZOIC EVOLUTION OF GEOMORPHIC AND SEDIMENTARY ENVIRONMENTS IN THE TIANSHUI-QIN'AN REGIONS[A];[C];2008
7 CHANG Hua-jin~(1,2,3),CHU Xue-lei~(1,2),WANG Jin-rong~4, FENG Lian-jun~(1,2),HUANG Jing~(1,2,3) (1 Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029, China;2.Key Lab of Mineral Resources,Chinese Academy of Sciences,Beijing 100029, China;3.Graduate University of the Chinese Academy of Sciences,Beijing 100049,China; 4.School of Earth and Environmental Sciences,Lanzhou University,Lanzhou 730000,China);Cu-Au M interalization of Adakite Belt in the Eastern Section of the North Qilian[A];[C];2009
8 Li Yuejun~1 Wu Genyao~1 Meng Qinglong~1 Yang Haijun~2 H an Jianfa~2 L i Xin sheng~2 Dong Lisheng~2 (1.Institute of Geology and Geophysics,Chinese Acadany of Sciences,Beijing 100029; 2.Tarin Oilfield Branch Company,China National Petroleum Corp,Korla,Xinjiang 841000);Fault system s in centralarea of the Tarin Basin:geometry,kinematics and dynamic settings[A];[C];2009
9 YONG Yong~(1,2),XIAO Wen-jiao~1,YUAN Chao~3,LI Ji-liang~1,YAN Zhen~4,MAO Qi-gui~(1,2) (1.State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences, Beijing,100029,China;2.Earth Sciences College,Graduate University of Chinese Academy of Sciences,Beijing,100039, China;3.Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou,GuangDong,510640,China; 4.Institute of Geology,Chinese Academy of geological Science,Beijing,100037,China);LA-ICPMS ZIRCON U-PB AGES OF GRANITIC PLUTONS FROM THE EASTERN SECTOR OF THE CENTRAL QILIAN AND THEIR GEOLOGIC IMPLICATION[A];[C];2009
10 Z.T.Guo~1,B.Sun~(1,2),Z.S.Zhang~(1,3),S.Z.Peng~1,G.Q.Xiao~4,J.Y.Ge~4,Q.Z.Hao~1,Y.S.Qiao~1,M.Y.Liang~1, J.F.Liu~1,Q.Z.Yin~1,and J.J.Wei~1 1 Key Laboratory of Cenozoic Geology and Environment,Institute of Geology and Geophysics,Chinese Academy of Sciences,P.O.Box 9825,Beijing,100029,China 2 Shandong Institute and Laboratory of Geological Sciences,Jinan,250013,China 3 Nansen-Zhu International Research Center,Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing, 100029,China 4 State Key Laboratory of Loess and Quaternary Geology,Institute of Earth Environment,Chinese Academy of Sciences,P.O. Box 17,Xian,710075,China;A major reorganization of Asian climate by the early Miocene[A];[C];2009
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7 THE MAGNETOTELLURIC SOUNDING GROUP, THE SEISMOLOGIcAL BRIGADE OF LANZHOU, NATIONAL SEISMOLOGICAL BUREAU;ON THE ELECTRIC CONDUCTIVITY CHARACTERISTICS OF THE NORTHERN PORTION OF THE NORTH-SOUTH EARTHQUAKE BELT OF CHINA[J];Chinese Journal of Sinica;1976-01
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10 ZHANG Qi ①, SUN Xiaomeng ②, ZHOU Dejin ① QIAN Qing ①, CHEN Yu③, WANG Yueming ④ JIA Xiuqin ⑤, HAN Song ⑤ (①Institute of Geology, Chinese Academy of Sciences, Beijing 100029;②Engineering and Technology College, Science and Techn;THE CHARACTERISTICS OF NORTH QILIAN OPHIOLITES, FORMING SETTINGS AND THEIR TECTONIC SIGNIFICANCE[J];ADVENCE IN EARTH SCIENCES;1997-04
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