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《地质科学》 2000-01
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THE NORTH QILIAN OCEANIC BASIN OF THE EARLY PALEOZOIC AGE: AN AULACOGEN OR A LARGE OCEANIC BASIN: A DISCUSSION WITH GE XIAOHONG

Zhang Qi Wang Yan Qian Qing (Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029)  
It is debated whether the north Qilian oceanic basin of the early Paleozoic age is an aulacogen or a large oceanic basin. Imprints preserved in ophiolites probably representing a large ocean are discussred in the paper. It is proposed that the north Qilian Orogen of the early Paleozoic between North China block and Qaidam block is a plate accretion melange belt, which consists of relict oceanic lithosphere, subducted complex and island arc-accreted wedge (or a few remnant micro-continental blocks). It is pointed that the north Qilian ophiolites are of Cordillera type, implying that the north Qilian was probably a large-scale ocean basin in early Paleozoic, not an aulacogen, and North China block and Qaidam block were very small at that time, being micro-continental blocks in vast ocean.
【Fund】: 国家自然科学基金
【CateGory Index】: P545
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10 LI Xiang-dong1,2,HE You-bin2,LIU Xun1,YOU Guo-qing,WANG Dan3,ZHENG Zhao-chang4(1.Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100038,China;2.School of Geoscience,Yangtze University,Jingzhou 434023,Hubei,China;3.Prtrochina Coalbed Methane Co.,Ltd.,Beijing 100013,China;4.Ningxia Bureau of Geology and Mineral Resources,Yinchuan 751104,Ningxia,China);An analysis of the tectonic setting of Xujiajuan Formation of Middle Ordovician Xiangshan Group in Ningxia[J];Geology in China;2011-02
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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 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
3 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
4 QIU Zhen and WANG QingChen 1.State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.Graduate School of Chinese Academy of Sciences,Beijing 100049,China;Geochemistry and sedimentary background of the Middle-Upper Permian cherts in the Xiang-Qian-Gui region[A];[C];2011
5 Yang Jingsui,Wu Cailai,Xia Linqi, Fan Qicheng,Xu Yigang,Xu Xisheng;Achievement and Prospect of Igneous Rock Petrology[A];[C];2006
6 Zhongjie Zhang~(a,*),Zhiming Bai~a,S.L.Klemperer~b,Xiaobo Tian~a,Tao Xu~a,Yun Chen~a,Jiwen Teng~a a State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing,China b Department of Geophysics,Stanford University,Stanford,CA 94305-2215,USA;Crustal structure across northeastern Tibet from wide-angle seismic profiling:Constraints on the Caledonian Qilian orogeny and its reactivation[A];[C];2014
7 WANG Lu-bo;DAI Shuang;ZHANG Li-li;ZHANG Xiang;LI Rong-xi;ZHANG Rui;ZHANG Ming-zhen;Research School of Arid Environment and Climate Change,Lanzhou University;Key Laboratory of Western China's Environmental Systems of Ministry of Education,Lanzhou University;Geological Survey of Gansu Province;School of Earth Science and Resources,Chang'an University;;Study on Geological Characteristics and Fluid Inclusion of Jiagongtai Gold Deposit in Gansu[A];[C];2014
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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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