Lithologic Reservoirs ›› 2019, Vol. 31 ›› Issue (5): 24-33.doi: 10.12108/yxyqc.20190503

• PETROLEUM GEOLOGY • Previous Articles     Next Articles

Characteristics of seismites and their geological significance of the upper fourth member of Shahejie Formation in Western Sag, Liaohe Depression

ZHAO Qingfeng1,2,3, ZHANG Jianguo1,2,3, KANG Wenjun1,2,3, WANG Siqi1, JIANG Zaixing1, DU Kefeng4, HUANG Changwu5   

  1. 1. School of Energy Resources, China University of Geosciences(Beijing), Beijing 100083, China;
    2. Key Laboratory of Marine Reservoir Evolution and Hydrocarbon Enrichment Mechanism, Ministry of Education, Beijing 100083, China;
    3. Key Laboratory of Strategy Evaluation for Shale Gas, Ministry of Land and Resources, Beijing 100083, China;
    4. Research Institute of Yanchang Petroleum(Group) Company Limited, Xi'an 710075, China;
    5. PetroChina Research Institute of Petroleum Exploration and Development, Beijing 100083, China
  • Received:2019-02-26 Revised:2019-05-06 Online:2019-09-21 Published:2019-09-16

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Abstract: In order to study the development characteristics and geological significance of the seismites of the upper fourth member of Shahejie Formation in Western Sag of Liaohe Depression,core observation and description,thin section identification and restoration of paleo-magnitude were carried out. The results show that:(1) Nine kinds of brittle plastic deformation structures such as liquefied veins,liquefied breccia,liquefied crinkled deformation,annular bedding,mounds and troughs,vein structure and syn-sedimentary fault formed in the finegrained sedimentary rocks of the upper fourth member of Shahejie Formation in Western Sag.(2)vertical vibration sequence of the seismites in the study area from bottom to top is as follows:shattered rock bed,liquefied crinkled deformation interval,interval of syn-sedimentary fault,interval of ball-and-pillow structure and vein structure,liquefied crinkled deformation interval and normal homogenized overlying bed.(3)The paleo-magnitude restoration based on sedimentary structures shows that the set of seismites was formed in earthquake events on the Richter scale at magnitude 5-8. Micro-fissures and faults caused by seismic events provided effective seepage channels for hydrocarbon migration,and a large number of dissolved pores developed around the channel. It has a certain improvement effect on the dense fine-grained carbonate reservoir in the study area. The research results show new fields and directions for the next oil and gas exploration in the Western Sag.

Key words: seismites, paleo-earthquake magnitude, seismites sequence, upper fourth member of Shahejie Formation, Western Sag, Liaohe Depression

CLC Number: 

  • TE122.2
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