Pore structure evolution and geological controls in lacustrine shale systems with implications for marine shale reservoir characterization
Understanding pore structure evolution in lacustrine shale systems provides critical insights for marine shale reservoir characterization. This study presents an integrated petrological and petrophysical analysis of a representative lacustrine shale succession, employing low temperature nitrogen ads...
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| Published in | Scientific reports Vol. 15; no. 1; pp. 17702 - 14 |
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| Main Authors | , , , , , , |
| Format | Journal Article |
| Language | English |
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London
Nature Publishing Group UK
21.05.2025
Nature Publishing Group Nature Portfolio |
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| Abstract | Understanding pore structure evolution in lacustrine shale systems provides critical insights for marine shale reservoir characterization. This study presents an integrated petrological and petrophysical analysis of a representative lacustrine shale succession, employing low temperature nitrogen adsorption (LTNA), whole rock X-ray diffraction (XRD), and scanning electron microscopy (SEM). The study shows that (1) Clay-dominated pore systems evolve through distinct pathways compared to marine shales, with illite/smectite mixed-layer minerals generating abundant mesopores through diagenetic transformation. (2) Organic matter- dominated pores display limited connectivity due to Type III kerogen characteristics and hydrocarbon generation-induced pore occlusion, contrasting with marine shale systems dominated by Type II kerogen. (3) Comparative analysis demonstrates that lacustrine shales preserve 30–40% higher micro-mesopore volumes than their marine counterparts under similar thermal maturity conditions, attributed to enhanced clay mineral diagenesis in freshwater environments. These findings provide a new framework for understanding pore structure development in non-marine depositional systems and provide valuable analogs for marine shale reservoir evaluation, particularly in transitional marine-lacustrine basins. |
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| AbstractList | Understanding pore structure evolution in lacustrine shale systems provides critical insights for marine shale reservoir characterization. This study presents an integrated petrological and petrophysical analysis of a representative lacustrine shale succession, employing low temperature nitrogen adsorption (LTNA), whole rock X-ray diffraction (XRD), and scanning electron microscopy (SEM). The study shows that (1) Clay-dominated pore systems evolve through distinct pathways compared to marine shales, with illite/smectite mixed-layer minerals generating abundant mesopores through diagenetic transformation. (2) Organic matter- dominated pores display limited connectivity due to Type III kerogen characteristics and hydrocarbon generation-induced pore occlusion, contrasting with marine shale systems dominated by Type II kerogen. (3) Comparative analysis demonstrates that lacustrine shales preserve 30–40% higher micro-mesopore volumes than their marine counterparts under similar thermal maturity conditions, attributed to enhanced clay mineral diagenesis in freshwater environments. These findings provide a new framework for understanding pore structure development in non-marine depositional systems and provide valuable analogs for marine shale reservoir evaluation, particularly in transitional marine-lacustrine basins. Understanding pore structure evolution in lacustrine shale systems provides critical insights for marine shale reservoir characterization. This study presents an integrated petrological and petrophysical analysis of a representative lacustrine shale succession, employing low temperature nitrogen adsorption (LTNA), whole rock X-ray diffraction (XRD), and scanning electron microscopy (SEM). The study shows that (1) Clay-dominated pore systems evolve through distinct pathways compared to marine shales, with illite/smectite mixed-layer minerals generating abundant mesopores through diagenetic transformation. (2) Organic matter- dominated pores display limited connectivity due to Type III kerogen characteristics and hydrocarbon generation-induced pore occlusion, contrasting with marine shale systems dominated by Type II kerogen. (3) Comparative analysis demonstrates that lacustrine shales preserve 30-40% higher micro-mesopore volumes than their marine counterparts under similar thermal maturity conditions, attributed to enhanced clay mineral diagenesis in freshwater environments. These findings provide a new framework for understanding pore structure development in non-marine depositional systems and provide valuable analogs for marine shale reservoir evaluation, particularly in transitional marine-lacustrine basins.Understanding pore structure evolution in lacustrine shale systems provides critical insights for marine shale reservoir characterization. This study presents an integrated petrological and petrophysical analysis of a representative lacustrine shale succession, employing low temperature nitrogen adsorption (LTNA), whole rock X-ray diffraction (XRD), and scanning electron microscopy (SEM). The study shows that (1) Clay-dominated pore systems evolve through distinct pathways compared to marine shales, with illite/smectite mixed-layer minerals generating abundant mesopores through diagenetic transformation. (2) Organic matter- dominated pores display limited connectivity due to Type III kerogen characteristics and hydrocarbon generation-induced pore occlusion, contrasting with marine shale systems dominated by Type II kerogen. (3) Comparative analysis demonstrates that lacustrine shales preserve 30-40% higher micro-mesopore volumes than their marine counterparts under similar thermal maturity conditions, attributed to enhanced clay mineral diagenesis in freshwater environments. These findings provide a new framework for understanding pore structure development in non-marine depositional systems and provide valuable analogs for marine shale reservoir evaluation, particularly in transitional marine-lacustrine basins. Abstract Understanding pore structure evolution in lacustrine shale systems provides critical insights for marine shale reservoir characterization. This study presents an integrated petrological and petrophysical analysis of a representative lacustrine shale succession, employing low temperature nitrogen adsorption (LTNA), whole rock X-ray diffraction (XRD), and scanning electron microscopy (SEM). The study shows that (1) Clay-dominated pore systems evolve through distinct pathways compared to marine shales, with illite/smectite mixed-layer minerals generating abundant mesopores through diagenetic transformation. (2) Organic matter- dominated pores display limited connectivity due to Type III kerogen characteristics and hydrocarbon generation-induced pore occlusion, contrasting with marine shale systems dominated by Type II kerogen. (3) Comparative analysis demonstrates that lacustrine shales preserve 30–40% higher micro-mesopore volumes than their marine counterparts under similar thermal maturity conditions, attributed to enhanced clay mineral diagenesis in freshwater environments. These findings provide a new framework for understanding pore structure development in non-marine depositional systems and provide valuable analogs for marine shale reservoir evaluation, particularly in transitional marine-lacustrine basins. |
| ArticleNumber | 17702 |
| Author | Gao, Xiaodan Li, Hu Wang, Haijun He, Shun Xie, Jiatong Xu, Ziqiang Qin, Qirong |
| Author_xml | – sequence: 1 givenname: Hu surname: Li fullname: Li, Hu email: lihu860628@126.com, lihu@suse.edu.cn organization: School of Economics, Sichuan University of Science and Engineering, State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Southwest Petroleum University), Sichuan Engineering Technology Research Center for High Salt wastewater Treatment and Resource Utilization, Sichuan University of Science and Engineering, Sichuan Key Provincial Research Base of Intelligent Tourism, Sichuan University of Science and Engineering, School of Geoscience and Technology, Southwest Petroleum University – sequence: 2 givenname: Ziqiang surname: Xu fullname: Xu, Ziqiang organization: CNPC Tarim Oilfield Branch Company – sequence: 3 givenname: Xiaodan surname: Gao fullname: Gao, Xiaodan email: gaoxiaodan@suse.edu.cn, gaoxiaodan92@naver.com organization: School of Economics, Sichuan University of Science and Engineering, Sichuan Key Provincial Research Base of Intelligent Tourism, Sichuan University of Science and Engineering – sequence: 4 givenname: Jiatong surname: Xie fullname: Xie, Jiatong organization: Sinopec Exploration Company – sequence: 5 givenname: Qirong surname: Qin fullname: Qin, Qirong organization: State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Southwest Petroleum University), School of Geoscience and Technology, Southwest Petroleum University – sequence: 6 givenname: Haijun surname: Wang fullname: Wang, Haijun organization: School of Economics, Sichuan University of Science and Engineering, Sichuan Key Provincial Research Base of Intelligent Tourism, Sichuan University of Science and Engineering – sequence: 7 givenname: Shun surname: He fullname: He, Shun organization: School of Geoscience and Technology, Southwest Petroleum University |
| BackLink | https://www.ncbi.nlm.nih.gov/pubmed/40399384$$D View this record in MEDLINE/PubMed |
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| Keywords | Unconventional reservoirs Lacustrine shale Nitrogen adsorption analysis Pore structure evolution Diagenetic controls |
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| Title | Pore structure evolution and geological controls in lacustrine shale systems with implications for marine shale reservoir characterization |
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