Lithologic Reservoirs ›› 2022, Vol. 34 ›› Issue (6): 47-59.doi: 10.12108/yxyqc.20220604

• PETROLEUM EXPLORATION • Previous Articles     Next Articles

Pore structure characteristics and genetic mechanism of Triassic Chang 7 shale oil reservoir in Longdong area

WEN Zhigang1,2, LUO Yushu1,2, LIU Jiangyan3, ZHAO Chunyu4, LI Shixiang3, TIAN Weichao1,2, FAN Yunpeng1,2, GAO Heting1,2   

  1. 1. Hubei Key Laboratory of Petroleum Geochemistry and Environment(Yangtze University), Wuhan 430100, China;
    2. Key Laboratory of Exploration Technologies for Oil and Gas Resources(Yangtze University), Ministry of Education, Wuhan 430100, China;
    3. Research Institute of Exploration and Development, PetroChina Changqing Oilfield Company, Xi' an 710018, China;
    4. No. 11 Oil Production Plant, PetroChina Changqing Oilfield Company, Qingyang 745100, Gansu, China
  • Received:2022-05-08 Revised:2022-05-31 Online:2022-11-01 Published:2022-11-09

Abstract: The pore structure characteristics of Chang 7 shale oil reservoir were characterized by high pressure mercury injection(HPMI), low-temperature nitrogen adsorption(LTNA), and nuclear magnetic resonance(NMR), and the effects of dominant diagenesis on pore structure were discussed. The results show that: (1)The shale oil reservoir of Triassic Chang 7 member in Longdong area is mainly feldspathic lithic sandstone and lithic arkose, with an average porosity of 7.55% and an average permeability of 0.149 mD,belonging to typical ultra-low porosity and ultra-low permeability reservoir. The reservoir space types are mainly dissolved pores, residual intergranular pores and clay intercrystalline pores, and a small amount of micro fractures are developed.(2)The reservoir is characterized by high displacement pressure, ranging from 0.67 MPa to 27.54 MPa, with an average of 5.54 MPa low maximum mercury saturation, ranging from 33.22% to 84.35%, with an average of 64.71%, and small average throat radius, ranging from 0.008 μm to 0.163 μm, with an average of 0.277 μm., showing strong heterogeneity. (3)The isotherms of the typical samples in the study area are all in an inverse S shape, belonging to a typical type Ⅳ isotherm. The type of hysteresis loop is dominated by type H3,indicating that the shape of pores less than 200 nm is mainly parallel plate shape.(4)The pore diameter of Chang 7 shale oil reservoir in the study area is mostly less than 30 μm. With the improvement of physical properties of samples,the proportion of larger pores (greater than 200 nm)in the reservoir increases gradually.(5)The shale oil reservoir of Chang 7 member in the study area has experienced three types of diagenesis: strong compaction, weak cementation and weak dissolution. Cementation and compaction have a negative effect,and dissolution has a constructive effect on the improvement of reservoir quality and pore structure.

Key words: microscopic pore structure, genesis, genetic mechanism, shale oil reservoir, Chang 7 member, Triassic, Longdong area, Ordos Basin

CLC Number: 

  • TE122.2
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