Characteristics and implications of micro-lithofacies in lacustrine-basin organic-rich shale: a case study of Jiyang depression, Bohai Bay Basin

被引:0
|
作者
Liu H. [1 ]
Yu B. [2 ]
Xie Z. [3 ]
Han S. [2 ]
Shen Z. [2 ]
Bai C. [2 ]
机构
[1] Oil and Gas Exploration Management Center, Sinopec Shengli Oilfield Company, Dongying, 257000, Shandong
[2] School of Earth Sciences and Resources, China University of Geosciences, Beijing
[3] Research Institute of Exploration and Development, Sinopec Shengli Oilfield Company, Dongying, 257000, Shandong
来源
Shiyou Xuebao/Acta Petrolei Sinica | 2018年 / 39卷 / 12期
关键词
Bohai Bay Basin; Jiyang depression; Micro-lithofacies; Shahejie Formation; Shale oil;
D O I
10.7623/syxb201812002
中图分类号
学科分类号
摘要
Shale oil is an important component of unconventional hydrocarbon resources, and is also a hot spot in research of petroleum geology. In China, shale oil resources massively occur in the continental lacustrine basin. Due to the differences between shale oil and conventional oil in reserving, sealing, trapping and migration, the lithofacies have a significant controlling effect on shale oil accumulation. This study focuses on organic-rich shale in the lower sub-member of Member 3 to upper sub-member of Member 4 of Shahejie Formation in Jiyang depression, Bohai Bay Basin. Based on the petrology, whole-rock X-ray diffraction (XRD), total organic carbon (TOC) content and direct hydrocarbon indication (DHI) of the study layers, it is indicated that the micro-lithofacies of shale layers are dominated by thin lenticle crystalline limestone micro-lithofacies (LF1), lamellar micritic limestone micro-lithofacies (LF2), thick massive lime mudstone micro-lithofacies (LF3), massive mudstone micro-lithofacies (LF4)and black shale micro-lithofacies (LF5). Among them, the favorable micro-lithofacies (or combination)for shale oil accumulation are LF5, LF4 and LF1+LF5. There are two shale oil accumulation models in Jiyang depression: one is the "self-generation and self-reservoir" model dominated by LF4 and LF5; the other is the "crystalline limestone reservoir" model dominated by LF1+LF5. The crystalline limestones are more beneficial to shale oil accumulation, development and production, and the LF1+LF5 is the "sweet spot" micro-lithofacies combination for continental shale oil exploration and development in Jiyang depression. © 2018, Editorial Office of ACTA PETROLEI SINICA. All right reserved.
引用
收藏
页码:1328 / 1343
页数:15
相关论文
共 50 条
  • [1] Zou C., Yang Z., Cui J., Et al., Formation mechanism, geological characteristics and development strategy of nonmarine shale oil in China, Petroleum Exploration and Development, 40, 1, pp. 14-26, (2013)
  • [2] Loucks R.G., Ruppel S.C., Mississippian Barnett shale: lithofacies and depositional setting of a deep-water shale-gas succession in the Fort Worth Basin, Texas, AAPG Bulletin, 91, 4, pp. 579-601, (2007)
  • [3] Abouelresh M.O., Slatt R.M., Lithofacies and sequence stratigraphy of the Barnett shale in east-central Fort Worth Basin, Texas, AAPG Bulletin, 96, 1, pp. 1-22, (2012)
  • [4] Monzon O., Yang Y., Kim J., Et al., Microbial fuel cell fed by Barnett shale produced water: power production by hypersaline autochthonous bacteria and coupling to a desalination unit, Biochemical Engineering Journal, 117, pp. 87-91, (2016)
  • [5] Fairbanks M.D., Ruppel S.C., Rowe H., High-resolution stratigraphy and facies architecture of the Upper Cretaceous (Cenomanian-Turonian)Eagle Ford Group, Central Texas, AAPG Bulletin, 100, 3, pp. 379-403, (2012)
  • [6] Denne R.A., Hinote R.E., Breyer J.A., Et al., The cenomanian-turonian eagle ford group of south texas: insights on timing and paleoceanographic conditions from geochemistry and micropaleontologic analyses, Palaeogeography, Palaeoclimatology, Palaeoecology, 413, pp. 2-28, (2014)
  • [7] Yu B., Classification and characterization of gas shale pore system, Earth Science Frontiers, 20, 4, pp. 211-220, (2013)
  • [8] Zhao W., Li J., Yang T., Et al., Geological difference and its significance of marine shale gases in South China, Petroleum Exploration and Development, 43, 4, pp. 499-510, (2016)
  • [9] Zhai G., Wang Y., Bao S., Et al., Major factors controlling the accumulation and high productivity of marine shale gas and prospect forecast in Southern China, Earth Science, 42, 7, pp. 1057-1068, (2017)
  • [10] Burton D., Woolf K., Sullivan B., Lacustrine depositional environments in the Green River Formation, Uinta Basin: expression in outcrop and wireline logs, AAPG Bulletin, 98, 9, pp. 1699-1715, (2014)