Slope Belts of Paleouplifts Control the Pore Structure of Organic Matter of Marine Shale: A Comparative Study of Lower Cambrian Rocks in the Sichuan Basin

Wang, Pengfei; Zhang, Chen; Liu, Aoran; Zhang, Pengfei; Qiu, Yibo; Li, Xin; Yu, Shanshan; Yao, Shuqing; Liu, Sanyi; Jiang, Zhenxue

doi:10.1155/2021/5517655

Cited by 1 publication

(1 citation statement)

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“…The amount of gaseous hydrocarbons, the number of OM pores, the pore diameter, and the regularity of the form increase with the length of the hydrocarbon-generation development. The integrated reservoir is enriched by a high number of gaseous hydrocarbons that have a lot of efficient storage space (OM pores) [55,56]. On the other hand, if the shale does not have enough time for the creation of hydrocarbons, not enough gaseous hydrocarbons, and not enough OM pores can be produced, preventing the large-scale accumulation of shale gas.…”

Section: Shale Gas Exploration Potential Analysismentioning

confidence: 99%

Shale Gas Exploration and Development Potential Analysis of Lower Cambrian Niutitang Formation and Lower Silurian Longmaxi Formation in Northwestern Hunan, South China, Based on Organic Matter Pore Evolution Characteristics

Miao,

Wang,

et al. 2023

JMSE

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Shale gas production is obviously higher within the Silurian Longmaxi Formation than that of the Cambrian Niutitang Formation according to the drilling test results in the northwest Hunan area. To clarify the reasons behind this variation, core samples from the two sets of shales were studied for a comprehensive comparison and analysis of their organic matter (OM) pore structure. Methods were used, including the total organic carbon content test, the vitrinite reflectance test, X-ray diffraction, and focused ion-beam scanning electron microscopy (FIB-SEM). The results show that these two shales have similar reservoir characteristics, both with abundant organic matter and high content of brittle minerals. However, the Longmaxi shale with 2.3% to 3.0%Ro presents lower thermal maturity than the Niutitang shale with over 3.0%Ro. In the case of pore structure associated with OM, a huge difference exists between the two shales. The OM pore shape of the Longmaxi shale is very regular, being mostly round and oval, while the OM pore shape of the Niutitang shale is irregular, being flat with a thin middle and thick and elongated ends. An important factor affecting OM pore evolution is thermal maturity. In turn, the thermal maturity is controlled by the tectonic evolution process, especially the maximum paleo-burial depth. In conclusion, the paleo-burial depth of the Lower Cambrian Niutitang shale in northwest Hunan is too large, which leads to the excessive evolution of organic matter in the shale, and the physical and chemical properties are similar to graphite, which leads to the disappearance of OM pores. Shale gas has no effective reservoir space and is largely dispersed in geological history. At the same time, due to the insufficient hydrocarbon-generation evolution time of the Lower Silurian Longmaxi Formation shale in this area, the shale could not form enough gaseous hydrocarbons and a large amount of effective reservoir space (OM pores with regular shape and large pore size), and finally failed to become a gas reservoir. Therefore, the exploration and development potential of the marine shale gas of the Lower Cambrian Niutitang Formation and the Lower Silurian Longmaxi Formation in northwest Hunan is poor.

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Section: Shale Gas Exploration Potential Analysismentioning

confidence: 99%