泥页岩中有机质：类型、热演化与有机孔隙

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doi:10.3799/dqkx.2022.130

Volume 48 Issue 12

Dec. 2023

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Liu Bei, 2023. Organic Matter in Shales: Types, Thermal Evolution, and Organic Pores. Earth Science, 48(12): 4641-4657. doi: 10.3799/dqkx.2022.130

Citation:

Liu Bei, 2023. Organic Matter in Shales: Types, Thermal Evolution, and Organic Pores. Earth Science, 48(12): 4641-4657. doi: 10.3799/dqkx.2022.130

Liu Bei, 2023. Organic Matter in Shales: Types, Thermal Evolution, and Organic Pores. Earth Science, 48(12): 4641-4657. doi: 10.3799/dqkx.2022.130

Citation:

Liu Bei, 2023. Organic Matter in Shales: Types, Thermal Evolution, and Organic Pores. Earth Science, 48(12): 4641-4657. doi: 10.3799/dqkx.2022.130

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Organic Matter in Shales: Types, Thermal Evolution, and Organic Pores

doi: 10.3799/dqkx.2022.130

Liu Bei^{1, 2
,
,}

1.
Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan 430074, China
2.
School of Earth Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2022-01-19
Available Online: 2024-01-03
Publish Date: 2023-12-25

Abstract

Abstract

Organic matter (OM) in mudstones/shales is the source of oil and gas, the organic petrographic classification of which has not reached a consensus. Traditional coal petrological methods do not fully apply to dispersed organic matter (DOM) in shales. OM-hosted pores are important constituents of the pore system in shale reservoirs, and they, to a large degree, control the gas content and porosity of shales. However, the origin of organic pores and their relationships with OM type and thermal maturity remain controversial. This study systematically summarized the types of DOM in shales, thermal evolution of different types of OM, and factors controlling the formation and preservation of organic pores, and proposed the issues related to DOM study and future research directions. DOM in shales can classified into five maceral groups: vitrinite, inertinite, liptinite, zooclasts, and secondary organic matter, with each group consisting of multiple macerals. Different macerals have different origins, and varying potential of hydrocarbon generation and development of organic pores. Organic pores in shales can be primary or secondary, the latter of which is the dominant type. Secondary organic pores occur in solid bitumen or pyrobitumen, and their development is related to thermal maturation of oil-prone macerals. The development of secondary organic pores is controlled by OM type and thermal maturity, and their preservation depends on thermal maturity, OM content, mineralogical composition of shales, and pore pressure. When conducting source rock evaluation, the hydrocarbon generation potential of OM should be studied based on a good understanding of maceral types, composition, and their hydrocarbon generation potential. In order to accurately assess the contribution of organic pores to the pore system of shale reservoirs, the influence of OM type, content, and thermal maturity should be taken into consideration.
- dispersed organic matter,
- shale,
- maceral,
- thermal evolution,
- solid bitumen,
- organic pores,
- petroleum geology

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References(134)

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Organic Matter in Shales: Types, Thermal Evolution, and Organic Pores

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