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《Acta Scicentiarum Naturalum Universitis Pekinesis》 2004-06
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Discussion on Mesozoic-Cenozoic Evolution of Tian Shan and Its Adjacent Basins

FANG Shihu 1),2) GUO Zhaojie 1) ZHANG Zhicheng 1) WU Chaodong 1) ( 1)Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, Peking University,Beijing,100871; 2)The Research Institute of Petroleum Exploration and Development,PetroChina,Beijing,100083)  
This paper discussed the main Mesozoic-Cenozoic tectonic-events, basin evolution, thermochronology and crustal shortening of Tian Shan and its adjacent basins.The basins of south and north Tian Shan have underwent various dynamics stages in Mesozoic-Cenozoic era.The Mesozoic-Cenozoic strata in the basins of south and north Tian Shan showed much information about tectonic evolution. Conglomeratic sedimentation of the latest Jurassic-earliest Cretaceous is consistent with the amalgamation at south margin of Eurasia block, and that of late Cenozoic is related to the India-Asia collision during late Oligocene to early Miocene. So far, the thermochronology data about Mesozoic-Cenozoic cooling events can be divided into three stages: early cretaceous, late Oligocene-Miocene and after Pliocene. These thermochronology data is the direct notes of tectonics events in the latest Jurassic-earliest Cretaceous and late Cenozoic. Tian Shan rose quickly during these two periods. Sedimentologic and thermochronological information proved that Tian Shan Area was active in tectonics during the latest Jurassic-earliest Cretaceous and late Cenozoic, which were the signs of transformation of basin types. Tarim basin and Junggar basin have the same evolution history: intra-continent faulted-depression basin in Jurassic, intra-continent depression basin from Cretaceous to Eocene, and Rejuvenated foreland basin form Neocene to Quaternary. The deformation of Tian Shan was propagating form west to east, which have illustrated by rate of crustal shortening, time-transgression of Xiyu Conglomerate, and GPS observations. The differential deformation of Tian Shan was related to northward extrusion of Pamir Syntaxis.
【Fund】: 国家重点基础研究规划项目 (2 0 0 1CB4 0 980 4 )
【CateGory Index】: P542
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Chinese Journal Full-text Database 10 Hits
1 Liu Zhihong 1) ,Lu Huafu 2) ,Jia Chengzao 3) ,Hu Zhongquan 4) ,Xu Xiaoxing 5) ( 1) Changchun University of Science and Technology, Changchun 130026;2) Nanjing University, Nanjing 210093;3) Tarim Petroleum Exploration and Development;STRUCTURAL CHARACTERISTICS AND ITS RELATION WITH HYDROCARBON OF KELASU TECTONIC ZONE IN KUQA FORELAND BASIN[J];JOURNAL OF CHANGCHUN UNIVERSITY OF SCIENCE AND TECHNOLOGY;1999-03
2 Li Zhongquan, Zhang Shouting, Wang Honghui (Chengdu University of Technology, China) Deng Gao (Engineering Geophysics Technique Company of South China);STRUCTURE GENETIC MECHANISM AND OIL GAS ACCUMULATION IN THE SOUTH BOADER OF JUNGGAR BASIN, XINJIANG, CHINA[J];JOURNAL OF CHENGDU UNIVERSITY OF TECHNOLOGY;1997-02
3 HE Bochu;TAN Keren;WU Oianhong(Changsha institute of Geotectonics,Academia Sinica,Changsha,410013);AGES AND Sr,Nd ISOTOPIC EVIDENCES OF MANTLE SOURCE MAGMATITE IN THE BU′S GOLD DEPOSIT,JIMUNAI COUNTY,NORTHERN XINJIANG[J];GEOTECTONICA ET METALLOGENIA;1994-03
4 Wang Qi and You Xinzhao (Institute of Seismology, China Seismological Bureau, Wuhan 430071) Wang Wenyin and Yang Zhiqiang (Xi’an College of Engineering, Xi’an);GPS MEASUREMENT AND CURRENT CRUSTAL MOVEMENT ACROSS THE HIMALAYA[J];CRUSTAL DEFORMATION AND EARTHQUAKE;1998-03
5 Zhang Qianfeng; Hu Aiqin;Zhang Guoxin;Fan Sikun and Pu Zhiping (Guangzhou Branch, Institute,of Geochemistry,Academia Sinica,Guangzhou 5 10640) Li Qixin (No. 1 Regional Geological Survey, Xinjiang Bureau of Geology and Mineral Resources);EVIDENCE FROM ISOTOPIC AGE FOR PRESENCE OF MESOZOIC-CENOZOIC MAGMATIC ACTIVITIES IN ALTAI REGION,XINJIANG[J];GEOCHIMICA;1994-03
6 Chen Jiangfeng; Man Fasheng; Ni Shoubin(Department of Earth and Space Sciences, China University of Science and Technology,Hefei 230026, China);NEODYMIUM AND STRONTIUM ISOTOPIC GEOCHEMISTRY OF MAFIC-ULTRAMAFIC INTRUSIONS FROM QINBULAKE ROCK BELT,WEST TIANSHAN MOUNTAIN,XINJIANG[J];GEOCHIMICA;1995-02
7 Zhao Zhenhua; Wang Zhonggang; Zou Tianren; A. Masuda(Guangzhou Institute of Geochemisiry, Chinese Academy of Sciences, Guangzhou 510640)(Institute of Geochemistry, CAS, Guiyang 550002)(Institute of Ore Deposit Geology, CAGS, Beijing 100037)(Department of;STUDY ON PETROGENESIS OF ALKALI-RICH INTRUSIVE ROCKS OF ULUNGUR, XINJIANG[J];GEOCHIMICA;1996-03
8 Ma Xingyuan (Institute of Geology, State Seismological Bureau);ON EXTENSIONAL TECTONICS[J];;1982-03
9 Liu Hefu (China University of Geosciences, Beijing 100083);DYNAMIC CLASSIFICATION OF SEDIMENTARY BASINS AND THEIR STRUCTURAL STYLES[J];;1993-06
10 Liu Hefu (Department of Energy Resources Geology, China University of Geosciences, Beijing 100083)Liang Huishe (Hebei College of Geology, Shijiazhuang 050031)Cai Liguo (Department of Energy Resources Geology, China University of Geosciences, Beijing 100083)Xia Yiping (Third Geophysical Survey Division, BGP, CNCP, Zhengding 050800)Liu Liqun (Institute of Petroleum Geology, MGMR, Beijing 100083);Evolution and Structural Style of Tianshan and Adjacent Basins, Northwestern China[J];;1994-06
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