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Structural Evolution of Chepaizi Uplift and its Control on Stratigraphic Deposition in the Western Junggar Basin, China

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Acta Geologica Sinica(English Edition) 2019年第4期93卷 1060-1075页

作者： NI Minjie CHEN Shi LIU Zichao SHANG Fengkai QI Jiafu WANG Lishuang State Key Laboratory of Petroleum Resources and Prospecting China University of PetroleumBeijing 102249China College of Geosciences China University of PetroleumBeijing 102249China Exploration and Development Research Institute Shengli Oilfield CompanySINOPECDongying 257015ShandongChina

Geological mapping,interpreted cross sections,structural analyses and residual thickness maps were used to characterize the evolution of stress setting,structure and stratigraphic distribution of the Chepaizi Uplift,which is a NW-SE trending structure located in the Western Junggar *** NS-trending faults show an important transpressional phase during the Late Permian,as demonstrated by tectonic stress field and stratigraphic thickness variations.A major compressional thrusting and strike-slip phase during the Late Jurassic created a series of NW-SE faults that originated by the large-scale uplift event in the northern *** were reactivated as thrust and dextral strike-slip *** addition,the angular unconformity observed between Jurassic and Cretaceous provide evidence of this tectonic *** of normal faults indicate that the area records southward tilting and regional derived extensional stress that took place during the *** that,thick Early Cenozoic strata are widely *** balanced cross-section highlights the evolution of stress setting and stratigraphic distribution of the Chepaizi Uplift.

关键词： structural evolution seismic section Junggar Basin Chepaizi Uplift northern tianshan

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