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《Journal of Jiling University (Earth Science Edition)》 2005-01
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Discussion on the Formation and Origin of the Shiguai Mesozoic Rift Basin in Inner Mongolia

XU Xiang-jun~(1),ZHAO Yu-jun~(2)(1.College of Earth Sciences, Jilin University, Changchun 130061,China; 2.Geophysical Exploration Institute of Heilongjiang Pro-(vince), Harbin 150036,China)  
The Shiguai Mesozoic fault basin is located in the front of the Daqingshan thrust system. Its formation and development was controlled by the early Jurassic extension and late Jurassic compression. According to crustal deformation characteristics, the evolution of this rift basin can be divided into three stages: early-middle Jurassic Wudanggou stage was featured mainly by crustal extension deformation with rapid deposit filling in the basin and the formation of a very thick coal-bearing detrial rock succession; the middle Jurassic Changhangou stage was featured by a stable tectonic environment during which the rift basin saw the deposition of mudstone and fresh limestone of coastal shallow lake faices; late Jurassic stage underwent strongly compression deformation in south-north direction and saw the formation of syntectonic foreland compression basin, in which a set of amaranth-gray amaranth coarse detrial rocks were deposited. Hence, important information on the crustal deformation is recorded in the internal litho-facies change, characteristics of sedimentary formations and strata contact relations in basin.
【Fund】: 中国地质调查局区域地质调查项目(200113000021)
【CateGory Index】: P544.4
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