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准噶尔盆地构造演化与动力学背景再认识
  
关键词:Junggar basin  foreland basin systems  pressure-flexure action  dynamic setting tectonic evolution
基金项目:“973”项目(编号:2003BA613A-02)
作者单位E-mail
吴孔友 石油大学地球资源与信息学院山东东营257061 wky990104@sohu.com 
查明 石油大学地球资源与信息学院山东东营257061  
王绪龙 新疆油田公司勘探开发研究院新疆克拉玛依834000  
曲江秀 石油大学地球资源与信息学院山东东营257061  
陈新 新疆油田公司勘探开发研究院新疆克拉玛依834000  
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摘要:
Further Researches on the Tectonic Evolution and Dynamic Setting of the Junggar Basin
      There still exist some different opinions concerning the evolution of Junggar basin, an important oil-bearing basin in wes-tern China. An analysis of geophysical data shows that geological structures of Junggar basin in plane and in profile have the foreland basin features. Based on the dynamic setting, the authors utilized the foreland basin systems and pressure-flexure action to divide the evolution of the Junggar basin into five stages: ① collision-basin-forming stage; ② pressure-flexure stage; ③ flexure-depression stage; ④ depression-sedimentation stage and ⑤ foreland basin regeneration stage. From Carboniferous to Permian, the ocean troughs around Junggar massif were closed early or late and continent-continent collision took place. At first, the northeastern part was formed during the late period of Early Carboniferous. Then Kelameili orogenic belt was developed in the northwest during middle and late periods of Late Carboniferous. Finally, the southern part was formed during the late period of Early Permian. With the uplift of marginal mountains, three foreland basin systems were formed in Juggar basin. From Triassic to Palaeogene, the plate squeezing action weakened and Junggar basin gradually entered a depression-subsidence phase from the intense compressive phase. From Neogene to Quaternary, North Tianshan Mountains were uplifted quickly and extensively under the influence of Himalayan movement. The southern part subsided again and formed the regenerated foreland basin from west to east. As a result of such a complex evolution, Junggar basin developed more than one sets of source-reservior-caprock assemblages and multiple periods of hydrocarbon accumulation, which provided favorable conditions for oil and gas accumulation.
WU Kong-you,ZHA Ming,WANG Xu-long,QU Jiang-xiu,CHEN Xin.2005.Further Researches on the Tectonic Evolution and Dynamic Setting of the Junggar Basin[J].Acta Geoscientica Sinica,26(3):217-222.
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