ORIGINAL RESEARCH article
Front. Earth Sci.
Sec. Sedimentology, Stratigraphy and Diagenesis
Volume 13 - 2025 | doi: 10.3389/feart.2025.1583053
Differences in microporous fractal characteristics of tight sandstones of different diagenetic facies: Chang 6 reservoirs of the Triassic Yanchang Formation in the western Ordos Basin, China
Provisionally accepted
- 1Lanzhou City University, Lanzhou, China
- 2Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences (CAS), Lanzhou, Gansu Province, China
- 3Lanzhou University, Lanzhou, Gansu Province, China
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Microporous structures of tight sandstones show diverse fractal features in different diagenetic facies. Experimental tests such as cast thin sections, scanning electron microscopy, high-pressure mercury pressure, and low-temperature nitrogen adsorption were applied to clarify the pore fractal differences between various diagenetic facies. The diagenesis, pore types, and pore distribution characteristics of typical tight sandstone samples from the Chang 6 reservoir of the Triassic Yanchang Formation in the Ordos Basin, China, are systematically analyzed. Furthermore, fractal theory is applied to investigate the differences in pore fractal characteristics among various diagenetic facies, as well as the controlling factors influencing these differences. The results show that within the study area, we have meticulously divided the diagenetic facies into four main categories: strong compaction facies, carbonate cementation facies, clay mineral cementation facies, weak cementation, and strong dissolution facies. Samples from different diagenetic facies exhibit significant variability in pore size distribution, and the microscopic pores structure is multifractal, with different fractal dimensions for different aperture ranges. The highest fractal dimension of different pores in strong compaction facies indicates strong compaction facies pore surface roughness. The pores are not regular enough and are unfavorable to the storage and infiltration of natural gas in the pores, followed by the carbonate cementation facies and the clay mineral cementation facies. The weak cementation and strong dissolution facies have a low fractal dimension. The pores are relatively more regular, which is more favorable to the storage and infiltration of the pores. Mineral compositions, reservoir properties, and sedimentary facies influence the pore fractal of the tight sandstone in the study area. This study reveals the relationship between diagenetic facies and pore fractals in tight sandstone reservoirs. The study is significant for exploring and developing tight oil in the study area.
Keywords: Diagenetic facies, Microscopic pores, Fractal features, Tight sandstone, Yanchang formation, Western Ordos basin
Received: 25 Feb 2025; Accepted: 18 Jun 2025.
Copyright: © 2025 Chen, Zhao, Zheng, Wang, Ma, Jia, Han and Gao. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
* Correspondence: Dayou Chen, Lanzhou City University, Lanzhou, China
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