Journal of Jilin University(Earth Science Edition) ›› 2017, Vol. 47 ›› Issue (6): 1695-1704.doi: 10.13278/j.cnki.jjuese.201706109

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Multiple Phase Deformation of Gumudi Anticline at South Margin of Junggar Basin

Ma Delong1,2,3, He Dengfa1, Wei Dongtao2,3, Wang Yanjun2, Wei Cairu2   

  1. 1. School of Energy Resources, China University of Geosciences, Beijing 100083, China;
    2. Research Institute of Petroleum Exploration and Development-Northwest, PetroChina, Lanzhou 730020, China;
    3. Key Laboratory of Reservoir Description, PetroChina, Lanzhou 730020, China
  • Received:2017-03-24 Online:2017-11-26 Published:2017-11-26
  • Supported by:
    Supported by National Natural Science Foundation of China (40739906) and National Science and Technology Major Project (2016ZX05003002)

Abstract: The Gumudi anticline is located at the north border of Fukang thrust belt, north piedmont zone of Bogeda Mountains. Combining with the outcrops, seismic and apatite fission track, we discussed the tectonic response of the sedimentary basin during the uplift of Bogeda Mountains. Vertically, the Gumudi anticline has dual structures:the layers below the Jurassic (J2x) Xishanyao formation were formed in 150-130 Ma and 100-80 Ma; while Xishanyao formation (J2x) and the above were formed in 30 Ma, with the features of propagation folds under faults breaking through. The results reflect that the multiple uplifts of Bogeda Mountains occurred after Late Jurassic, and the dual structure formation was formed earlier with shallower burial depth. The Gumudi anticline is a favorable area for oil and gas exploration in future.

Key words: south margin of Junggar basin, Bogeda Mountains, Gumudi anticline, multiple phases of deformation, oil and gas exploration

CLC Number: 

  • 618.13
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