Pore Structure Characterization of Lacustrine Shale and its Coupling Relationship with Sedimentary Structure from the Upper Cretaceous Qingshankou Formation, Southern Songliao Basin, NE China
Author:
Funder
the National Key Research and Development Programs of China
Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
https://link.springer.com/content/pdf/10.1007/s13369-023-08402-7.pdf
Reference71 articles.
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2. Gou, Q.Y.; Xu, S.; Hao, F.; Shu, Z.G.; He, S.; Wu, Z.R.: Differences in the nanopore structure of organic-rich shales with distinct sedimentary environments and mineral compositions. Energy & Fuels. 35, 16562–16577 (2021)
3. Zhu, X.M.; Zhang, M.Z.; Zhu, S.F.; Dong, Y.L.; Li, C.; Bi, Y.Q.; Ma, L.: Shale Lithofacies and Sedimentary Environment of the Third Member, Shahejie Formation, Zhanhua Sag, Eastern China. Acta Geologica Sinica - English Edition. 96, 1024–1040 (2022)
4. Zhang, J.; Jia, Y.; Du, G.: Diagenesis and its effect on reservoir quality of Silurian sandstones, Tabei area, Tarim Basin China. Petroleum Sci. 4, 1–13 (2007)
5. Han, H.; Guo, C.; Zhong, N.; Pang, P.; Gao, Y.: A study on fractal characteristics of lacustrine shales of Qingshankou Formation in the Songliao Basin, northeast China using nitrogen adsorption and mercury injection methods. J. Petrol. Sci. Eng. 193, (2020)
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