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《Journal of Changchun University of Science and Technology》 2001-04
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MESOZOIC OROGENIC MOVEMENT AND TECTONIC EVOLUTION IN DAQINGSHAN REGION, INNER MONGOLIA

XU Zhong_yuan, LIU Zheng_hong, YANG Zhen_sheng (College of Earth Sciences, Jilin University, Changchun 130061, China)  
Daqingshan is located in the western part of Yinshan-Yanshan intraplate orogenic belt, its tectonic outline and structural pattern were formed by crust polytectonic deformation in Mesozoic. Indosinian movement was a strong pressed folding orogenic movement in company with magma activity, which was dominated by N-S direction compression. Crust compresive deformation, dominating also in early Yanshan stage, formed Daqingshan thrust system and controlled the formation and development of foreland basin which occurred in front of Daqingshan thrust system. Crust deformation of middle Yanshan stage was extension, which was resulted by the changes of region tectonic stress field and gravity action, and formed early Cretaceous Baotou-Huhehaote extensional basin. Late Yanshan stage was compressive crust deformation which not only formed the wedge-type thrust structure but also caused upper Cretaceous Series unconformable contact with lower Cretaceous Series.
【Fund】: 原地质矿产部内蒙古大青山地区 1∶5万 ( 6幅 )区域地质调查项目 ( 0 1992 0 90 3 1)
【CateGory Index】: P542.2
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3 Zhou Lingdi;Zhao Zhenhua;Zhou Guofu(Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640);ISOTOPIC CHRONOLOGY OF SOME ALKALINE ROCK BODIES IN CHINA[J];GEOCHIMICA;1996-02
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5 Ye Junlin Xiang Shuyuan ( China University of Geosciences, Wuhan 430074 );THE CHARACTERISTICS AND FORMATION MECHANISM OF THRUST-NAPPE STRUCTURE IN MAGMATIC BODY AREA IN CHICHENG, HEBEI PROVINCE[J];;1989-01
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10 W. H. WONG The Geological Survey of China;CRUSTAL MOVEMENTS AND IGNEOUS ACTIVITIES IN EASTERN CHINA SINCE MESOZOIC TIME.1[J];;1927-01
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