Multiscale Characteristics and Controlling Factors of Shale Oil Reservoirs in the Permian Lucaogou Formation (Jimusaer Depression, Junggar Basin, NW China)

被引:1
作者
Lian, Yang [1 ]
Zhang, Liping [1 ]
Chen, Xuan [1 ]
Tao, Xin [1 ]
Deng, Yuhao [1 ]
Li, Peiyan [1 ]
机构
[1] Yangtze Univ, Sch Geosci, Wuhan 430100, Peoples R China
基金
中国国家自然科学基金;
关键词
multiscale characterization; lithofacies; channel lobe sedimentary architecture; hyperpycnal flows; shale oil reservoir; Lucaogou formation; GRAINED SEDIMENTARY-ROCKS; TIGHT OIL; JIMSAR SAG; ACCUMULATION; MODEL;
D O I
10.3390/min15050438
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The Permian Lucaogou Formation (PLF) shale oil reservoirs in the Junggar Basin exhibit significant lithological heterogeneity, which limits the understanding of the relationship between macroscopic and microscopic reservoir characteristics, as well as insights into reservoir quality. To address this gap, thirty core samples, exhibiting typical sedimentary features, were selected from a 46 m section of the PLF for sedimentological analysis, thin section examination, high-performance microarea scanning, and scanning electron microscopy. Seven main lithofacies were identified, including massive bedding slitstone/fine-grained sandstone (LS1), cross to parallel bedding siltstone (LS2), climbing ripple laminated argillaceous siltstone (LS3), paired graded bedding argillaceous siltstone (LS4), irregular laminated argillaceous siltstone (LS5), irregular laminated silty mudstone (LM2), and horizontal laminated mudstone (LM2). The paired graded bedding sequences with internal erosion surfaces, massive bedding, and terrestrial plant fragments suggest a lacustrine hyperpycnal flow origin. The channel subfacies of hyperpycnal flow deposits, primarily consisting of LS1 and LS2, reflect strong hydrodynamic conditions, with a single-layer thickness ranging from 1.3 to 3.8 m (averaging 2.2 m) and porosity between 7.8 and 14.2% (averaging 12.5%), representing the primary sweet spot. The lobe subfacies, composed mainly of LS3, LS4, and LS5, reflect relatively strong hydrodynamic conditions, with a single-layer thickness ranging from 0.5 to 1.4 m (averaging 0.8 m) and porosity between 4.2 and 13.8% (averaging 9.6%), representing the secondary sweet spot. In conclusion, strong hydrodynamic conditions and depositional microfacies are key factors in the formation and distribution of sweet spots. The findings of this study are valuable for identifying sweet spots in the PLF and provide useful guidance for the exploration of lacustrine shale oil reservoirs in the context of hyperpycnal flow deposition globally.
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页数:23
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