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Article

Lithofacies Types and Pore Structure Characteristics of Marine Shale in the Lower Cambrian Shuijingtuo Formation, Middle Yangtze Region, China

1
School of Energy Resources, China University of Geosciences (Beijing), Beijing 100083, China
2
State Key Laboratory of Deep Earth Processes and Resources, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
*
Author to whom correspondence should be addressed.
J. Mar. Sci. Eng. 2025, 13(7), 1292; https://doi.org/10.3390/jmse13071292
Submission received: 8 June 2025 / Revised: 27 June 2025 / Accepted: 28 June 2025 / Published: 30 June 2025
(This article belongs to the Section Geological Oceanography)

Abstract

The lithofacies and pore structural characteristics of shale reservoirs directly affect the exploration and development of shale gas. To clarify the exploration and development potential of the Lower Cambrian Shuijingtuo Formation (SJT) shale in the Middle Yangtze region, China, this study employs integrated experimental approaches, including optical and scanning electron microscopy (SEM) observations, X-ray diffraction (XRD) mineralogical analysis, and low-pressure gas (N2/CO2) adsorption, to classify mudstone lithofacies within the SJT and elucidate pore structural characteristics and dominant geological control across different lithofacies. The research results show that (1) Six main types of shale lithofacies are found in the STJ, including low-TOC massive calcareous mudstone (LMCM), low-TOC laminated mixed mudstone (LLMM), medium-TOC massive mixed mudstone (MMMM), high-TOC massive mixed mudstone (HMMM), high-TOC laminated siliceous mudstone (HLSM), and laminated argillaceous mudstone (LAM). (2) The pore types of SJT mudstone primarily include organic pores, intragranular clay mineral pores, and microfractures. The pore structure of mudstone is mainly controlled by clay mineral content and TOC content. However, the controlling factors of pore structure vary among different mudstone lithofacies. LMCM and LLMM are dominated by intragranular clay mineral pores, with their pore structures mainly controlled by clay mineral content. The pore types of HLMM and HLSM are organic pores, with pore structures predominantly controlled by TOC content. (3) The SJT mudstone gas reservoir exhibits diverse types, including HLSM, LAM, and LLMM. HLSM is characterized by the highest brittleness index and elevated pore volume (PV) and it can be considered the optimum lithofacies in the study area. Additionally, LLMM has the highest PV and relatively high brittleness index, positioning it as another significant reservoir target in the study area. Therefore, the Lower Cambrian shale gas reservoirs in the Middle Yangtze region exhibit diverse reservoir types. These research findings provide a scientific basis for the next phase of shale gas exploration planning in the Lower Cambrian.
Keywords: favorable lithofacies; organic pores; shale gas; Lower Cambrian; Middle Yangtze region favorable lithofacies; organic pores; shale gas; Lower Cambrian; Middle Yangtze region

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MDPI and ACS Style

Fan, J.; Liu, W.; Qian, Y.; Li, J.; Zhou, Q.; Gao, P. Lithofacies Types and Pore Structure Characteristics of Marine Shale in the Lower Cambrian Shuijingtuo Formation, Middle Yangtze Region, China. J. Mar. Sci. Eng. 2025, 13, 1292. https://doi.org/10.3390/jmse13071292

AMA Style

Fan J, Liu W, Qian Y, Li J, Zhou Q, Gao P. Lithofacies Types and Pore Structure Characteristics of Marine Shale in the Lower Cambrian Shuijingtuo Formation, Middle Yangtze Region, China. Journal of Marine Science and Engineering. 2025; 13(7):1292. https://doi.org/10.3390/jmse13071292

Chicago/Turabian Style

Fan, Jialin, Wei Liu, Yujing Qian, Jinku Li, Qin Zhou, and Ping Gao. 2025. "Lithofacies Types and Pore Structure Characteristics of Marine Shale in the Lower Cambrian Shuijingtuo Formation, Middle Yangtze Region, China" Journal of Marine Science and Engineering 13, no. 7: 1292. https://doi.org/10.3390/jmse13071292

APA Style

Fan, J., Liu, W., Qian, Y., Li, J., Zhou, Q., & Gao, P. (2025). Lithofacies Types and Pore Structure Characteristics of Marine Shale in the Lower Cambrian Shuijingtuo Formation, Middle Yangtze Region, China. Journal of Marine Science and Engineering, 13(7), 1292. https://doi.org/10.3390/jmse13071292

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