混积型页岩油储层甜点体特征及平面分布——以吉木萨尔凹陷芦草沟组为例
李大鹏 , 王喜鑫 , 李少华 , 陈玉琨 , 张嘉恩 , 胡凯
东北石油大学学报 ›› 2026, Vol. 50 ›› Issue (4) : 17 -29.
混积型页岩油储层甜点体特征及平面分布——以吉木萨尔凹陷芦草沟组为例
Characteristics and planar distribution of sweet spots in mixed-sedimentary shale oil reservoirs: a case study of the Lucaogou Formation in the Jimsar Sag
以准噶尔盆地吉木萨尔凹陷芦草沟组为例,利用岩心和测井资料,采用铸体薄片、X射线衍射、扫描电镜、纳米CT、高压压汞及氮气吸附等实验方法,分析甜点体储层岩石学特征、物性特征、混合沉积及差异成岩特征,划分甜点段沉积微相和成岩相类型,探讨甜点体主控因素并预测甜点体平面分布。结果表明:吉木萨尔凹陷芦草沟组甜点体主要由白云质粉砂岩、凝灰质粉砂岩及粉砂质白云岩等组成,属于超低-特低孔、超低渗储层;孔隙类型以粒内溶孔和粒间溶孔为主,主要为亚微米孔隙,孔喉连通性较好,孔隙形态主要为板状平行狭缝孔和半封闭楔形孔。甜点体的形成受沉积、成岩作用控制,陆源碎屑组分是影响甜点体发育的主控因素。砂质坝、砂质滩等微相主要发育陆源主导型混积岩,粒度较粗,颗粒分选好,杂基含量低,富集长石、凝灰质等易溶组分;抗压实作用强,后期经历较强的溶蚀作用,形成凝灰质-长石溶蚀相、混合胶结-溶蚀孔相和绿泥石薄膜-粒间孔相等优势成岩相。优势沉积微相与优质成岩相的叠合区为甜点体的有利发育区。该结果为准噶尔盆地混积型页岩油目标优选提供支持。
The Permian Lucaogou Formation in the Jimsar Sag, Junggar Basin, was investigated using core and well-log data, together with cast thin-section petrography, X-ray diffraction, scanning electron microscopy, nano-CT, high-pressure mercury intrusion, and nitrogen adsorption analyses. The petrological characteristics, reservoir properties, mixed-sedimentary features, and differential diagenesis of the sweet spot reservoirs were characterized. Sedimentary microfacies and diagenetic facies within the sweet spot intervals were identified, the controlling factors of sweet spot development were evaluated, and the planar distribution of the sweet spots was predicted. The results indicate that the sweet spot reservoirs in the Lucaogou Formation are mainly composed of dolomitic siltstone, tuffaceous siltstone, and silty dolostone, and are characterized by ultra-low to very low porosity and ultra-low permeability. The pore system is dominated by intragranular and intergranular dissolution pores, with submicron pores being the most abundant. The pore-throat networks are relatively well connected, and the pores are mainly plate-like parallel slit-shaped pores and semi-closed wedge-shaped pores. Sweet spot development is jointly controlled by depositional processes and diagenetic modification, among which terrigenous clastic input is the primary controlling factor. Sandy-bar and sandy-flat microfacies are dominated by siliciclastic-rich mixed sedimentary rocks characterized by relatively coarse grain size, good sorting, low matrix content, and abundant soluble components, including feldspar and tuffaceous material. These rocks have relatively high resistance to mechanical compaction and subsequently underwent strong dissolution, resulting in the development of favorable diagenetic facies, including tuffaceous-feldspar dissolution facies, mixed cementation-dissolution-pore facies, and chlorite-coating-intergranular-pore facies. Favorable zones for sweet spot development occur where favorable sedimentary microfacies overlap with favorable diagenetic facies. These results provide a geological basis for target selection in mixed-sedimentary shale oil exploration in the Junggar Basin.
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中国石油科技创新基金项目(2021DQ02-0106)
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