Lithologic Reservoirs ›› 2020, Vol. 32 ›› Issue (2): 14-23.doi: 10.12108/yxyqc.20200202

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Sedimentary characteristics and geological significance of earthquake events of Sha 3 member in Huimin Sag,Jiyang Depression

LIU Jianning1,2, HE Youbin1,2, WANG Ning1,2, GU Zhixiang1,2, HAO Ting3, LIU Yawei4   

  1. 1. School of Geosciences, Yangtze University, Wuhan 430100, China;
    2. Key Laboratory of Exploration Technologies for Oil and Gas Resources, Ministry of Education, Yangtze University, Wuhan 430100, China;
    3. Research Institute, China United Coalbed Methane Co., Ltd., Beijing 100000, China;
    4. Underground Operation Branch, Bohai Drilling Engineering Co., Ltd., Cangzhou 062550, Hebei, China
  • Received:2019-09-19 Revised:2019-10-23 Online:2020-03-21 Published:2020-01-19

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Abstract: In order to study the sedimentary characteristics of paleoearthquake events in the third member of Shahejie Formation in Huimin Sag of Jiyang Depression and its reservoir controlling effect,core observation,vertical sequence division of single well of seismic sedimentary rocks,analysis of main controlling factors of sedimentation and geological significance of paleoearthquake events were carried out. The results show that:(1)The structure of seismites is very well developed in the third member of Shahejie Formation in Huimin Sag, including shatter crack, autoclastic breccia,stepped small fault,liquefied vein,liquefied curl,liquefied breccia and other brittle plastic deformation structures.(2)Seismic intensity,sediment consolidation degree and terrain slope are the main factors affecting the development of seismites. The vertical sedimentary sequence of several wells shows that the development characteristics of seismites in different structural positions in the study area are different, which can be divided into four areas,namely near source gentle area,main seismic area,near source slope area and far source gentle area.(3)The study of earthquake event deposition provides a basis for the determination of fault activity rate, growth index and other parameters in Huimin Sag,and the seismic event is an important power source for stimulating the secondary migration of sand body. The vibration in seismic event can cause the particle rearrangement of unconsolidated sediments,and reduce the heterogeneity of the reservoir in the third member of Shahejie Formation.(4)The abundant brittle seismites near faults may be the auxiliary channel of oil and gas migration,the autoclastic breccia formed by earthquakes is a good reservoir,and the compacted layer with uniform liquefaction is a high-quality caprock. The results of this study are of great significance to seismic exploration in Huimin Sag.

Key words: paleoearthquake events, seismites, Sha 3 member, Huimin Sag, Jiyang Depression

CLC Number: 

  • P512.2
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