Volume 30 Issue 4
Aug.  2024
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Article Navigation >  Journal of Geomechanics  > 2024  >  30(4): 579-594
WANG Y P，BAO Z D，ZHANG L J，et al.，2024. Diagenesis of microbial dolomite reservoirs in the second Member of Dengying Formation of Ediacaran in the Penglai area, Sichuan Basin: Insights into the formation and evolution of high-quality reservoirs[J]. Journal of Geomechanics，30（4）：579−594 doi: 10.12090/j.issn.1006-6616.2024062
Citation: WANG Y P，BAO Z D，ZHANG L J，et al.，2024. Diagenesis of microbial dolomite reservoirs in the second Member of Dengying Formation of Ediacaran in the Penglai area, Sichuan Basin: Insights into the formation and evolution of high-quality reservoirs[J]. Journal of Geomechanics，30（4）：579−594 doi: 10.12090/j.issn.1006-6616.2024062
shu

Diagenesis of microbial dolomite reservoirs in the second Member of Dengying Formation of Ediacaran in the Penglai area, Sichuan Basin: Insights into the formation and evolution of high-quality reservoirs

doi: 10.12090/j.issn.1006-6616.2024062
  • 1.

    School of Geosciences, China University of Petroleum (Beijing), Beijing 102249, China

  • 2.

    Exploration and Development Research Institute, PetroChina Southwest Oil & Gasfield Company, Chengdu 610041, Sichuan, China

  • 3.

    Institute of Logging Technology and Engineering, Yangtze University, Jingzhou 434023, Hubei, China

Funds:  This research is co-funded by the National Key Research and Development Program of China (Grant No. 2018YFC0604304) and the Special Project of the Department of Science and Technology, Sinopec (Grant No. P23180).
More Information
  • Received: 2024-06-02
  • Revised: 2024-06-23
  • Accepted: 2024-07-01
    • Available Online: 2024-07-15
  • Published: 2024-08-28
    Abstract
  •   Objective  The microbial dolomite of the second Member of the Dengying Formation（Deng 2 Member） in the Penglai area of the Sichuan Basin is widely distributed and considered a potential target for deep carbonate oil and gas exploration. Unlike conventional high-quality reservoirs characterized by porosity and karst fractures, the carbonate rocks of the Deng 2 Member mainly consist of microbial dolomite. The genesis and diagenetic evolution of these high-quality reservoirs remain unclear.   Methods  This study employed petrographic thin sections, scanning electron microscopy (SEM), cathodoluminescence, and computed tomography （CT）scanning to conduct a detailed analysis of the microbial dolomite reservoirs in the Dengying Formation, using field outcrop and core samples. The aim was to gain a deeper understanding of the effects of diagenesis on pore formation and the development of high-quality reservoirs.   Results and Conclusion   The microbial carbonate reservoirs in the study area were characterized by low porosity and very low permeability, predominantly consisting of fracture-porosity (cavity) type microbial dolomite. The reservoir space was primarily composed of intergranular dissolution pores, residual framework dissolution pores, intragranular dissolution pores, and small to medium-sized dissolution cavities, with minor occurrences of intercrystalline pores and intercrystalline dissolution pores. The Deng 2 Member has undergone multiple diagenetic processes; penecontemporaneous dissolution and early epigenetic dissolution were key factors in enhancing porosity.   Significance   These findings enhance the understanding of the genesis of high-quality microbial carbonate reservoirs in the Ediacaran System of the Sichuan Basin and provide valuable information for deep oil and gas exploration and development in the region.

     

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