Full-Text Search:
Home|Journal Papers|About CNKI|User Service|FAQ|Contact Us|中文
《Geological Review》 2015-06
Add to Favorite Get Latest Update

The Intrusive Spatial——Temporal Evolutional Framework in the Paleo-Asian Tectonic Domain

DENG Jinfu;FENG Yanfang;DI Yongjun;LIU Cui;XIAO Qinghui;SU Shangguo;ZHAO Guochun;MENGFei;CHE Rufeng;State Key Laboratory of Geological Processes and Mineral Resources,Key Laboratory of Lithosphere Tectonics and Lithoprobing Technology of Ministry of Education,China University of Geosciences;Development and Research Center,Survey Bureaus of China Geological;  
For a long time a lot of the models about the tectonic evolution and the orogenic architecture of the Paleo-Asian tectonic domain are suggested by many famous geologists. However,there are large divergence of the views,especially about both the space distribution and the closing time of the Paleo-Asian Ocean. Based on the intrusive tectonic map of China with the scale of 1: 2500,000,by this paper we would like to join the discussion.( 1) The formation of the intrusive arc,and the collisional as well as the postorogenic igneous petrotectonic assemblages is occurred progressively younger from west to east with time,and the trend lines of the main tectonic zones is developed from near-east——west in the west to near-north——south directions in the east,both of which is suggested the transition of the Paleo-Asian Ocean closing to development of the Pacific tectonic domain.( 2) The broad trench—arc—basin system developed at the southern margin of the Siberia craton situated in the north of the main oceanic basin; the passive continental margin at the west,and the narrow trench—arc—basin system in the middle,as well as the active continental margin at the east,respectively,developed at the northern margin of the Tarim—North China craton.( 3) Both the remnant arc and the oφ since Pt3 is scattered within the main arc,and is regarded as the basement beneath the main arc.( 4) The classical "massif"in the orogenic zone is considered to be the remnant arc by this paper,because they are intrusive arc formed in the early stage during the oceanic subduction.( 5) The main oceanic basin is recognized from three signs by this paper,( a) The closing of the ocean is latest,( b) The oceanic subduction is bidirectional when the active arc at both the sides,or is developed at one side when one side is active continental margin,and the other side is passive continental margin,( c) The long-live and the residue ocean of the Mediterranean sea type are developed as the early stage of the continent——continent collision.( 6) A lot of both the intrusive arcs and the oφ during Pt3—T support the formation of the large amount of the juvenile continental crust by Sengor et al.,as well as is corresponded to the positive value of the εNd( t) for the granites,which,in turn,is suggested to be formation of the large amount of the oceanic subduction resulted in the cooling of the mantle,and the adding eclogites into the mantle,finally,the high density mantle flow is formed as the dynamic source for the closing of the Paleo-Asian Ocean and then the collision between the Siberia and the Tarim—North—China cratons.
【Fund】: 国家自然科学基金委员会和中国科学院“板块构造与大陆动力学”学科发展战略项目、“侵入岩大地构造重大关键地质问题研究”(编号:中地调研合同[2014]第169号)、“全国侵入岩成矿地质背景研究”(编号:中地调研合同[2012]第107号);; 中国地质调查局项目“内蒙古东部——黑龙江西部燕山期火成岩特征及其成矿意义”(编号:12120114020901)、“内蒙古中东部——黑龙江中生代岩浆作用与金(银)铜(钼)矿成矿作用研究”(编号:1212011121075)的成果
【CateGory Index】: P588.12
Download(CAJ format) Download(PDF format)
CAJViewer7.0 supports all the CNKI file formats; AdobeReader only supports the PDF format.
【Citations】
Chinese Journal Full-text Database 8 Hits
1 LI Jin-yi1,ZHANG Jin2,YANG Tian-nan1,LI Ya-ping3,SUN Gui-hua4,ZHU Zhi-xin5,WANG Li-jia11.Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China2.Institute of Geology,China Earthquake Administration,Beijing 100029,China3.Center of Development and Research,China Geological Surveys,Beijing 100037,China4.Guangzhou Marine Geological Survey,Ministry of Land and Resources,Guangzhou 510760,China5.Geological Research Academe of Xinjiang,Urumqi 830011,China;Crustal Tectonic Division and Evolution of the Southern Part of the North Asian Orogenic Region and Its Adjacent Areas[J];Journal of Jilin University(Earth Science Edition);2009-04
2 PAN Gui-tang~1 XIAO Qing-hui~2 LU Song-nian~3 DEN Jin-fu~4 FENG Yi-min~5 ZHANG Ke-xin~6 ZHANG Zhi-yong~2 WANG Fang-guo~1 XING Guang-fu~7 HAO Guo-Jie~3 FENG Yan-fang~2 (1.Chengdu Institute of Geology and Mineral Resources,Chengdu 610082,Sichuan,China;2.Development and Research Center of China Geological Survey,Beijing 100037,China;3.Tianjin Institute of Geology and Mineral Resources,Tianjin 300170,China; 4.China University of Geosciences,Beijing 100083,China;5.Xi'an Institute of Geology and Mineral Resources,Xi'an 710054,Shaanxi, China;6.State Key Laboratory of Geological Process and Mineral Resource,Wuhan 430074,Hubei,China; 7.Nanjing Institute of Geology and Mineral Resources,Nanjing 210016,Jiangsu,China);Subdivision of tectonic units in China[J];Geology in China;2009-01
3 Ma Wenpu(China University of Geosciences, Beijing, 100083);SOME IMPORTANT PROBLEMS ON CURRENT OROGEN RESEARCHING[J];EARTH SCIENCE FRONTIERS;1999-03
4 WANG Hong-zhen~ 1 , HE Guo-qi~ 2 , ZHANG Shi-hong~ 1 1.School of Earth Sciences and Resources,China University of Geosciences,Beijing 100083,China 2.Department of Geology,Peking University,Beijing 100875,China;The geology of China and Mongolia[J];Earth Science Frontiers;2006-06
5 YANG Wencai;SONG Haibin;State Key Lab of Continental Tectonics and Dynamics,Institute of Geology,Chinese Academy of Geological Sciences;Institute of Geology and Geophysics,Chinese Academy of Sciences;;Ocean—Continent Transition Process Reveled by Worldwide Comparison of Crust and Upper Mantle Structures[J];Geological Review;2014-01
6 DENG Jinfu;FENG Yanfang;DI Yongjun;LIU Cui;XIAO Qinghui;SU Shangguo;MENG Fei;MA Shuai;YAO Tu;State Key Laboratory of Geological Processes and Mineral Resources,Key Laboratory of Lithosphere Tectonics and Lithoprobing Technology of Ministry of Education,China University of Geosciences;Development and Research Center,Survey Bureaus of China Geological;;Magmatic Arc and Ocean—Continent Transition:Discussion[J];Geological Review;2015-03
7 MA Wenpu 1 ,LU Songnian 2 ,WANG Guosheng 1(1.China University of Geosciences,Beijing100083,China;2.Tianjin Institute of Geology and Mineral Resources,China Geological Survey,Tianjin300170,China);Tectonic positioning of the Islands of Japan in the Mesozoic Asian fron tier and its relation to the regional geology of eastern China[J];Regional Geology of China;2003-03
8 Li Jin-yi1,Qu Jun-feng1,Zhang Jin1,Liu Jian-feng1,Xu Wen-liang2,Zhang Shuan-hong3,Guo Rui-qing4,Zhu Zhi-xin5,Li Ya-ping6,Li Yong-fei7,Wang Tao1,Xu Xue-yi8,Li Zhi-pei8,Liu Yong-qing1,Sun Li-xin9,Jian Ping1,Zhang Yu10,Wang Li-jia1,Peng Shu-hua9,Feng Qian-wen1,Wang Yu1,Wang Hong-bo1,Zhao Xi-xi1 1.Institute of Geology,CAGS,Beijing 100037,China;2.College of Earth Sciences,Jilin University,Changchun 130061,JiLin,China;3.Institute of Geomechanics,CAGS,Beijing 100081,China;4.Geological and Mining Engineering Institute,Xinjiang University,Urumqi 830049,Xinjiang,China;5.Geological Research Academy of Xinjiang,Urumqi 830011,Xinjiang,China;6.Development and Research Center,China Geological Survey,Beijing 100037,China;7.Shenyang Center,China Geological Survey,Shengyang 110034,Liaoning,China;8.Xi’an Center,China Geological Survey,CGS,Xi’an 710054,Shanxi,China;9.Tianjin Center,China Geological Survey,Tianjin 300170,China;10.Institute of Regional Geological Survey of Heilongjiang Province,Haerbin 150080,Heilongjiang,China;New Developments on the Reconstruction of Phanerozoic Geological History and Research of Metallogenic Geological Settings of the Northern China Orogenic Region[J];Geological Bulletin of China;2013-Z1
【Co-citations】
Chinese Journal Full-text Database 10 Hits
1 WEI Dong,ZHONG Kanghui,SONG Xiaoqin,ZHAO Dekun,LIU Qingshuang(College of earth sciences,Chengdu university of technology,Chengdu 610059,China);The discussion about the geological characteristics and genesis of Naduonong pb-zn deposits in Tibet[J];Sichuan Nonferrous Metals;2011-03
2 SU Hu1,ZHONG Kanghui1,LIU Qingshuang1,ZHOU Huiwen2,WEI Dong1,GOU Jin3(1.College of earth sciences,Chengdu university of technology,Chengdu 610059,China;2.The geological survey institute of hainan province,Haikou 570206,China;3.Tibet institute ofgeological survey,Lasa 850007,China);Intrusive rocks building and metallogenesis of gold deposits of Pusong of Nimu County in Tibet[J];Sichuan Nonferrous Metals;2011-03
3 YUAN Feng,ZHOU Tao-fa ,YUE Shu-cang( Department of Resources and Environmental Science,Hefei University of Technology,Hefei 230009 China );GEODYNAMIC SETTING OF METALLIZATION OF GOLD AND MULTI-METAL IN THE NURT AREA,XINJIANG[J];Geology of Anhui;2001-02
4 LAN Xue-yi1,ZHOU Cun-ting2,WANG JIAN-wei3,TANG Zheng-jiang1,XU Wei2,DU Jian-guo2(1.Insitute of Exploration Technology of Anhui Province,Hefei,Anhui 230031,China;2.Institute of Geological Survey of Anhui Province,Hefei,Anhui 230001,China;3.Institute of Geophysical and Geochemical Exploration Technology of Anhui Province,Hefei,Anhui 230022,China);GRAVITATIONAL ANOMALY FEATURES ZONING AND GEO-STRUCTURAL UNITS DIVISION IN ANHUI PROVINCE[J];Geology of Anhui;2012-01
5 ZHAO Zehui GUO Zhaojie ZHANG Chen LU Jiemin (School of Earth and Space Sciences,Peking University,Beijing,100871);Tectonic Evolution of the Santanghu Basin,East Xinjiang and Its Implication for the Hydrocarbon Accumulation[J];Acta Scicentiarum Naturalum Universitis Pekinesis;2003-02
6 ZHENG Rongguo,WU Tairan,ZHANG Wen,XU Cao,MENG Qingpeng The Key Laboratory of Orogenic Belts and Crustal Evolution(MOE),School of Earth and Space Sciences,Peking University,Beijing 100871;Early Devonian Tectono-Magmatic Events in the Middle Beishan,Gansu Province:Evidence from Chronology and Geochemistry of Gongpoquan Granite[J];Acta Scientiarum Naturalium Universitatis Pekinensis;2012-04
7 LI Jing chao 1 ,WANG Shi cheng 2 ,YANG Yi heng 2 (1.China University of Geoscience, Beijing 100083,China;2.Jilin University, Changchun 130026,China);SYNTHETICAL INFORMATION RESEARCH FOR GIANT AND SUPER ORE DEPOSITS METALLOGENIC LAWS IN XINJIANG ALTAI METALLOGENIC PROVINCE[J];Journal of Changchun University of Science and Technology;2002-04
8 DING Qing-feng, SUN Feng-yue, Li Bi-le (College of Earth Sciences, Jilin University, Changchun130061, China);Evolution of Cenozoic collision orogen of north Kalimantan and its metallogenesis[J];Journal of Jiling University (Earth Science Edition);2004-02
9 XU Xue-chun,ZHENG Chang-qing,ZHAO Qing-ying(College of Earth Sciences, Jilin University, Changchun 130061, China);Metamorphic Types and Crustal Evolution of HercynianOrogenic Belt in Altai Region, Xinjiang[J];Journal of Jiling University (Earth Science Edition);2005-01
10 LI Jin-yi1,ZHANG Jin2,YANG Tian-nan1,LI Ya-ping3,SUN Gui-hua4,ZHU Zhi-xin5,WANG Li-jia11.Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China2.Institute of Geology,China Earthquake Administration,Beijing 100029,China3.Center of Development and Research,China Geological Surveys,Beijing 100037,China4.Guangzhou Marine Geological Survey,Ministry of Land and Resources,Guangzhou 510760,China5.Geological Research Academe of Xinjiang,Urumqi 830011,China;Crustal Tectonic Division and Evolution of the Southern Part of the North Asian Orogenic Region and Its Adjacent Areas[J];Journal of Jilin University(Earth Science Edition);2009-04
China Proceedings of conference Full-text Database 10 Hits
1 CAO Mingjian~(1,2),QIN KeZhang~1 and LI JiLiang~1 1.Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.Graduate School of Chinese Academy of Sciences,Beijing 100039,China;Research progress on the flat subduction and its metallogenic effect,two cases analysis and some prospects[A];[C];2012
2 ZHANG Xi~(1,2),GAO Jun~1,DONG LianHui~3,LI JiLei~(1,2),JIANG Tuo~(1,2),QIAN Qing~1 and SU Wen~1 1.Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.Graduate University of Chinese Academy of Sciences,Beijing 100049,China 3.The Bureau of Geology and Mineral Resources Development of Xinjiang,Urumqi 830000,China;Zircon LA-ICP-MS U-Pb age of I type granitoids from Qiaohuote copper deposit in Central Tianshan of Xinjiang and its geological implications[A];[C];2012
3 ZHU MingTian~1,WU Guang~(2,3**),XIE Hongjing~4,LIU Jun~2 and ZHANG LianChang~1 1.Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037,China 3.Lingbao Jinyuan Mining Limited Liability Company,Henan Province,Lingbao 472500,China 4.Key Laboratory of Mineralogy and Metallogeny,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640,China;Geochronology and geochemistry of the Kekesai intrusion in western Tianshan,NW China and its geological implications[A];[C];2012
4 GUO Zhi-hua,ZHANG Bao-lin~*,QI Min,JIA Wen-cheng, SHEN Xiao-li,HUANG Xue-fei (Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China);The application of high precision ground magnetic prospecting for geological mapping in the 13451 mining area in Mongolia[A];[C];2012
5 Yue Guoli,Li Wei,Yang Guisong,Zhao Ke,Dong Haimin (1.Henan Institute of Geological Survey,Zhengzhou,450001; 2.Regional Geological Surveying Party,Henan Bureau of Geological Exploration and Mineral Development,Zhengzhou,450001);Potential Exploration For Angzhang Lead-Zinc Mineralization in Tibet[A];[C];2009
6 Yue Guoli,Li Wei,Zhang Shaobo,Gao Ming,Cui Xiaofeng,Wang Fuquan (Henan Institute of Geological Survey,Zhengzhou 450001,Henan,China);Mineral Prospecting and Ore-bearing Potential Evaluation on Laigu Formation Rocks in Gangdishi Belt,Tibet[A];[C];2010
7 ZHANG Qi,ZHOU GuoQing and WANG Yan 1.Institute of Geology and Geophysics,Chinese Academy of Sciencnes,Bejing 100029,China 2.Department of Earth Sciences,Nanjing University,Nanjing 210083,China 3.Department of Earth Sciences,Hongkong University,Hongkong,China;The distribution of time and space of chinese ophiolites,and their tectonic settings[A];[C];2003
8 QIAN Qing,XU ShouLi,HE GuoQi,Reiner KLEMD,XIONG XianMing,LONG LingLi and GAO Jun 1.Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.Bureau of Jiang su Petroleum Survey,Yang zhou 225009 3.Kay Laboratory of Orogenic Belts and Crustal Evolution,Ministry of Education,School of Earth and Space Sciences,Peking University,Beijing, 100871,China 4.Mineralogisches Institut,Universit(a|¨)t W(u|¨)rzburg,Am Hubland 97074,W(u|¨)rzburg,Germany 5.College of Resources and tnvironmental Engineering,Guizhou University,Guigang 550003,China;Elemental geochemistry and tectonic significance of Cambrian basalts from the northern side of the Nalati Mountain.[A];[C];2008
9 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
10 LI GuangMing~1,SHEN YuanChao~1,LIU TieBing~1,SHEN Ping~1 and ZHOU NengWu~2 (1 Key Lab.of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029, China;2 No.11 Geological Party,Xinjiang Bureau of Geology and Mineral Exploration and Development,Changji 830000, Xinjiang,China);Metallogenic evolution of Tuokuzibayi gold deposit in southern Altay,north Xinjiang:Evidence from characteristics of quartz vein systems,isotopic geochemistry and Ar-Ar chronology[A];[C];2008
【Secondary Citations】
Chinese Journal Full-text Database 10 Hits
1 TANG Wenhao,ZHANG Zhicheng,LI Jianfeng,FENG Zhishuo,CHEN Chen The Key Laboratory of Orogenic Belts and Crustal Evolution(MOE),School of Earth and Space Sciences,Peking University,Beijing 100871;;Geochemistry of the Carboniferous Volcanic Rocks of Benbatu Formation in Sonid Youqi,Inner Mongolia and Its Geological Significance[J];Acta Scientiarum Naturalium Universitatis Pekinensis;2011-02
2 LIN Ying_dang 1, LIU Peng_ju 1, PENG Xiang_dong 1,LIU Dian_tao 2 (1.Changchun University of Science and Technology, Changchun 130026, China; 2.Gudong Factory of Shengli Oil Field, Dongying 257231, China);THE CORRELATION OF THE MIDDLE PERMIAN STRATA AND CHARACTORISTIC OF CORAL FAUNA IN NORTH CHINA[J];JOURNAL OF CHANGCHUN UNIVERSITY OF SCIENCE AND TECHNOLOGY;2000-04
3 LI Jin-yi1,ZHANG Jin2,YANG Tian-nan1,LI Ya-ping3,SUN Gui-hua4,ZHU Zhi-xin5,WANG Li-jia11.Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China2.Institute of Geology,China Earthquake Administration,Beijing 100029,China3.Center of Development and Research,China Geological Surveys,Beijing 100037,China4.Guangzhou Marine Geological Survey,Ministry of Land and Resources,Guangzhou 510760,China5.Geological Research Academe of Xinjiang,Urumqi 830011,China;Crustal Tectonic Division and Evolution of the Southern Part of the North Asian Orogenic Region and Its Adjacent Areas[J];Journal of Jilin University(Earth Science Edition);2009-04
4 Peng Xiangdong, Zhang Meisheng, Zhang Songmei (Chanchun University of Science and Technologe, Changchun 130026) Mi Jiarong (Tianjin Normal University, Tianjin 300070);THE DIVISSION AND ITS CHARACTERISTIC OF PERMIAN PALEOBIOGEOGRAPHY IN JILIN AND HEILONGJIANG OROGENIC BELT[J];JOURNAL OF CHANGCHUN UNIVERSITY OF SCIENCE AND TECHNOLOGY;1998-04
5 ZHANG Sen-gui,ZHANG Yun-bai and YAN Hui-jun Editorial Office of Journal of Stratigraphy,Nanjing Institute of Geology and Palaeontology,Chinese Academy of Scieoces,Nanjing 210008;A BRIEF INTRODUCTION TO THE "INTERNATIONAL STRATIGRAPHIC CHART"(2008)[J];Journal of Stratigraphy;2009-01
6 YIN Fuguang~1, PAN Guitang~1, LI Xingzhen~1, MENG Debao~2, BAI Daoyuan~2 and LIU Wei~2 (1. Chengdu Institute of Geology and Mineral Resources, Chengdu, SC 610081, China; 2. Hunan Institute of Geological Survey,Changsha, HN 410011, China);GEOLOGICAL AND GEOCHEMICAL CHARACTERISTICS OF THE OPHIOLITE COMPLEX IN THE CENTRAL SECTION OF THE KUNLUN MOUNTAINS[J];Geotectonica Et Metallogenia;2004-02
7 GUO Kun-yi 1,3 ,ZHANG Chuan-lin 1,3 ,ZHAO Yu 3 ,DONG Yong-guan 3 ,WANG Ai-guo 3 ,XIE Ya-ping 3(1.Department of Earth Sciences,Jilin University,Changchun130026,Jilin,China;2.Institute of Geochemistry,Chinese Academy of;Geochemistry of Meso-and Neoproterozoic intra-oceanic arc volcanic rocks in the eastern segment of the western Kunlun orogenic belt[J];Chinese Geology;2002-02
8 LI Cai1, HE Zhong-hua1, LI Hui-min2(1. College of Earth Sciences,Jilin University,Changchun 130061, Jilin, China;2. Institute of Geology and Minerals product,Tianjin 300170, China);U-Pb and Sm-Nd dating of mafic dike swarms in southern Qiangtang, Qinghai-Tibet Pleatau and its tectonic significance[J];Chinese Geology;2004-04
9 XIAO Qing-hui1,8, QIU Rui-zhao2,3, DENG Jin-fu4, LI Ting-dong3,5, MO Xuan-xue4, HONG Da-wei3, WANG Tao3, LU Xin-xiang6, WU Fu-yuan5,7, XIE Cai-fu8(1. Information Center of Ministry of Land and Resources, Beijing 1000812, China;2.Development and Research Center,China Geological Survey,Beijing 100037;3. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China;4. China University of Geosciences, Beijing 100083, China;5. College of Earth Science, Jilin University, Changchun 130061, Jilin, China;6. Henan Institute of Geology, Zhengzhou 450053, China;7.Institute of Geology and Geophysics,Chinese Academy of Science Beijing 100029,China;8. Yichang Institute of Geology and Mineral Resources, Yichang 443003, Hubei, China);Granitoids and continental crustal growth modes in China[J];Chinese Geology;2005-03
10 WU Bo1,2,HE Guo-qi1,WU Tai-ran1,LI Hui-jun1,3,LUO Hong-ling1(1.School of Earth and Space Sciences,Key Laboratory of Orogenic Belts and Crustal Evolution,Ministry of Education,Peking University,Beijing 100871,China;2.China National Petroleum Will Logging Technology Service Corp.Ltd.,Beijing 110043,China;3.Institute of Geomechanics,Chinese Academy of Geological Sciences 100081 Beijing,China);Discovery of the Buergen ophiolitic mélange belt in Xinjiang and its tectonic significance[J];Geology in China;2006-03
©2006 Tsinghua Tongfang Knowledge Network Technology Co., Ltd.(Beijing)(TTKN) All rights reserved