首页|陆相混积页岩不同岩相孔隙差异特征及影响机制——以吉木萨尔凹陷二叠系芦草沟组为例

陆相混积页岩不同岩相孔隙差异特征及影响机制——以吉木萨尔凹陷二叠系芦草沟组为例

Characteristics of pore differences between different lithofacies of continental mixed shale and the influencing mechanism:An example from the Permian Lucaogou Formation in the Jimusar Depression

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岩相对优质储层及有利含油区的分布起着决定性作用,为查明吉木萨尔凹陷二叠系芦草沟组页岩油储层不同岩相或岩相组合的储集特征和影响机制,综合运用全岩矿物X射线衍射分析(XRD)、总有机碳含量测定(TOC)、岩石薄片鉴定、镜质组反射率(R.)、场发射扫描电镜、低场核磁共振、高压压汞实验、低温氮气吸附实验以及物性分析等手段,研究了芦草沟组不同岩相孔隙差异特征及影响机制.结果表明:研究区主要发育的岩相包括高碳块状粉砂质砂屑云岩(HK-Ⅱ1)、高碳纹层状粉砂质泥页岩(HW-Ⅰ2)、富碳块状粉砂质砂屑云岩(RK-Ⅱ1)、富碳块状泥质粉砂岩(RK-Ⅲ2).页岩有机质生烃伴生的有机酸、碳酸溶蚀作用显著,催生了粒间孔、粒内孔和溶蚀缝的规模发育.不同页岩岩相的孔隙结构大小以及孔隙结构复杂程度存在明显差异.沉积环境和成岩作用相互之间的耦合、匹配关系是导致孔隙差异化发育的关键.
The lithology plays a decisive role in the distribution of high-quality reservoirs and fa-vorable oil-bearing areas.In order to find out the reservoir characteristics and influencing mecha-nism of different lithofacies or lithofacies combinations of shale oil reservoirs in Permian Lucao-gou Formation of Jimsar Sag,the whole rock mineral X-ray diffraction analysis(XRD),total organic carbon content determination(TOC),rock thin section identification,vitrinite reflec-tance(Ro),field emission scanning electron microscope,low field nuclear magnetic resonance,high pressure mercury injection experiment,low temperature nitrogen adsorption experiment and physical property analysis were used to study the difference characteristics and influencing mechanism of different lithofacies pores in Lucaogou Formation.The results show that:The main lithofacies in the study area include high-carbon massive silty sandy dolomite(HK-Ⅱ1),high-carbon laminated silty shale(HW-Ⅰ2),carbon-rich massive silty sandy dolomite(RK-Ⅱ1),and carbon-rich massive argillaceous siltstone(RK-Ⅲ 2).The organic acid and carbonate dissolution associated with hydrocarbon generation of shale organic matter were significant,which promoted the scale development of intergranular pores,intragranular pores and dissolu-tion fractures.There are obvious differences in pore structure size and complexity of different shale lithofacies.The coupling and matching relationship between sedimentary environment and diagenesis is the key to the differential development of pores.

mixed shaleLucaogou Grouplithofaciespore structurefractal dimension

贺小标、罗群、李鑫、李映艳、邓远、邱兆轩、韦波

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中国石油大学(北京)油气资源与探测国家重点实验室,北京 102249

中国石油大学(北京)非常规油气科学技术研究院,北京 102249

新疆大学地质与矿业工程学院,新疆乌鲁木齐 830047

中国石油新疆油田分公司勘探开发研究院,新疆克拉玛依 834000

新疆维吾尔自治区煤田地质局,新疆乌鲁木齐 830002

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混积页岩 芦草沟组 岩相 孔隙结构 分形维数

中国石油-中国石油大学(北京)战略合作科技专项

ZLZX2020-01-6

2024

中国矿业大学学报
中国矿业大学

中国矿业大学学报

CSTPCD北大核心
影响因子:1.83
ISSN:1000-1964
年,卷(期):2024.53(1)
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