Journal of Jilin University(Earth Science Edition) ›› 2020, Vol. 50 ›› Issue (2): 542-552.doi: 10.13278/j.cnki.jjuese.20190104

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Denudation Restoration and Structural Framework of Prototype Paleogene Basin in Tangyuan Fault Depression

Wu Jingfeng1,2, Meng Qi'an2, Fu Xiaofei1   

  1. 1. College of Earth Sciences, Northeast Petroleum University, Daqing 163318, Heilongjiang, China;
    2. Exploration and Development Research Institute of Daqing Oilfield Company Ltd., Daqing 163712, Heilongjiang, China
  • Received:2019-05-08 Online:2020-03-26 Published:2020-03-31
  • Supported by:
    Supported by National Science and Technology Major Project(2016E-0202)

Abstract: The structure of Tangyuan fault depression is complex,and its transformation is strong,which leads to the uncertainty of the original sedimentary subsidence center,and this, in turn, restricts the progress of oil and gas exploration. Starting from the calculation of denudation amount by using the stratigraphic trend method and the vitrinite reflectance method, the authors obtained the amount of stratum denudation of Baoquanling Formation,Dalianhe Formation, and Xin'ancun Formation, and restored the shape of the prototype basin in different periods combined with earthquake and structural features and the geological modeling technology. Through the calculation and recovery,it is considered that during Xin'ancun Formation period,the thickest part was in the eastern boundary,and the eastern sedimentary zone was formed by the influence of paleo-tectonics, and was divided by the middle uplift into two parts,the north and the south,the subsidence center was located in the middle section of the fault in the eastern boundary. During the Dalianhe Formation period,the two early subsidence zones gradually merged into one zone, the north of the eastern boundary,with some small subsidence zones in the west and south of the fault depression, and the thickest part was still located in the descending plate of the eastern fault zone. During the Baoquanling Formation period,the two early (eastern?) subsidence zones were completely merged into one zone,and the subsidence zone in the western part of the fault depression was formed and enlarged,thus the east and west subsidence centers were formed.On the above,the pattern of prototype basin,the distribution,and migration process of the sedimentation centers in different periods are finally clarified.

Key words: Tangyuan fault depression, denudation restoration, prototype basin, tectonic framework

CLC Number: 

  • TE121.2
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