Pore characteristics and influencing factors of the Lower Cambrian marine shale in the Lower Yangtze area

BAO Yanjun; ZHANG Penghui; CHEN Jianwen; LIANG Jie; MENG Xianghao; FU Yilin; XUE Lu; ZHANG Xu; WANG Baxiu

doi:10.16562/j.cnki.0256-1492.2021110201

Marine Geology & Quaternary Geology > 2022 > 42(2): 144-157. > DOI: 10.16562/j.cnki.0256-1492.2021110201

BAO Yanjun，ZHANG Penghui，CHEN Jianwen，et al. Pore characteristics and influencing factors of the Lower Cambrian marine shale in the Lower Yangtze area[J]. Marine Geology & Quaternary Geology，2022，42(2)：144-157. DOI: 10.16562/j.cnki.0256-1492.2021110201

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Pore characteristics and influencing factors of the Lower Cambrian marine shale in the Lower Yangtze area

1.
College of Oceanography, Hohai University, Nanjing 210024, China
2.
Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266237, China
3.
School of Resources and Environmental Engineering, HeFei University of Technology, Hefei 230009, China
4.
Laboratory for Marine Mineral Resources, Pilot National Laboratory for Marine Science and Technology, Qingdao 266237, China
5.
Qingdao Institute of Marine Geology, China Geological Survey, Qingdao 266237, China
6.
State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation (Chengdu University of Technology), Chengdu 610059, China

More Information

Received Date: November 01, 2021
Revised Date: November 23, 2021
Accepted Date: November 23, 2021
Available Online: April 13, 2022

Graphical Abstract

Abstract

Abstract

The marine shale samples of the Lower Cambrian Mufushan Formation collected from the Well GD1 in the Lower Yangtze area are systematically studied in this paper for pore structure characteristics and their influencing factors. Various testing methods, such as field emission scanning electron microscope, X-ray diffraction analysis, gas adsorption, high-pressure mercury injection and organic geochemical analysis are adopted for this research. It is revealed that the Mufushan shale is mainly composed of quartz, calcite and clay minerals in mineralogy. The total organic carbon content is quite high, and the organic matter is dominated by the type I of kerogen overmatured. The pores are dominated by matrix pores including intergranular and intragranular pores, organic matter pores and microfractures. Organic matter pores are well developed, and the proportion of intergranular pores is the highest. Organic matter abundance has certain influence on the pore size and specific surface area of organic matter pores. Compaction is the main factor for pore evolution in the overmatured stage, while rigid minerals, as supporting components, play a positive role in the preservation of organic matter pores. The fractal dimension has a good correlation with the total organic carbon content and specific surface area but weak correlation with pore volume, suggesting that the roughness of the pore wall and the complexity of the pore structure are affected by organic matter abundance.
- pore characteristics,
- shale,
- well GD1,
- Lower Cambrian,
- Lower Yangtze area

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References (60)

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Pore characteristics and influencing factors of the Lower Cambrian marine shale in the Lower Yangtze area