2023 Vol. 50, No. 2
Article Contents

ZHANG Qiong, XU Wenli, XU Xu, WEN Huaguo, ZHANG Linpu, GUO Gengsheng, HE Chuan. 2023. Reservior characteristics and main controlling factors of the third member of Paleogene Shahejie Formation in Fulin sag, Bohai Bay Basin[J]. Geology in China, 50(2): 543-556. doi: 10.12029/gc20191119002
Citation: ZHANG Qiong, XU Wenli, XU Xu, WEN Huaguo, ZHANG Linpu, GUO Gengsheng, HE Chuan. 2023. Reservior characteristics and main controlling factors of the third member of Paleogene Shahejie Formation in Fulin sag, Bohai Bay Basin[J]. Geology in China, 50(2): 543-556. doi: 10.12029/gc20191119002

Reservior characteristics and main controlling factors of the third member of Paleogene Shahejie Formation in Fulin sag, Bohai Bay Basin

    Fund Project: Supported by National Natural Science Foundation (No.41972109)
More Information
  • Author Bio: ZHANG Qiong, female, born in 1995, master, major in sedimentary geology; E-mail: 1093641810@qq.com
  • Corresponding author: XU Wenli, male, born in 1982, Ph.D, lecturer, engaged in reservoir sedimentology research; E-mail: 156613174@qq.com 
  • This paper is the result of oil and gas exploration engineering.

    Objective

    The third member of Shahejie Formation of the Paleogene is the most important oil and gas horizon in Fulin sag, Zhanhua sag, jiyang sag, Bohai Bay Basin, and it has the essential scientific and guiding significance of strengthening the reservoir characteristics of Shahejie Formation, analyzing the main controlling factors of the reservoir, and guiding the reservoir prediction and oil and gas exploration engineering and resources of Shahejie Formation in the area.

    Methods

    Based on the petrography and reservoir physical property data, this paper is aiming to dicipher the origin of the sandstone reservoirs of Paleogene Shahejie Formation the Zhanhua sag, Bohai Bay basin.

    Results

    The thin sections observation and sem analysis show that the lithofacies of the reservoirs are consist of feldspathic lithic sandstone and lithic feldspar sandstone, with low compositional and structural maturities, indicating that they rapidly deposited in the environment proximal to provenance. The reservoir space type of the reservoir is mainly residual primary intergranular pores, intergranular solution pores and intragranular solution pores, mainly low medium porosity and ultra-low permeability pore type reservoirs. The development of high-quality reservoirs is controlled by sedimentary microfacies and diagenesis. The sedimentary microfacies are the basis for the development of high-quality reservoirs, and cementation and dissolution are the key factors for the development of high-quality reservoirs.

    Conclusions

    (1) The rock types in the study area were mainly feldspathic lithic sandstone and lithic feldspar sandstone. (2) It is generally a low-to-mesoporous and ultra-low permeability reservoir; (3) High-quality reservoirs in the study area are mainly distributed in braided river delta distributary channels and estuarine bars; (4) Compaction and cementation are the main destructive diagenesis in the study, while dissolution has constructive diagenesis on reservoir physical properties.

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