首页|期刊导航|现代地质|南堡凹陷古近系沙河街组一段湖相块状与纹层状页岩储层微观特征差异性研究

南堡凹陷古近系沙河街组一段湖相块状与纹层状页岩储层微观特征差异性研究OA

Reservoir micro-characteristics of massive and laminated lacustrine shales:A comparative study from the Paleogene Shahejie Formation,Nanpu Sag

中文摘要英文摘要

为探讨湖相纹层状页岩和块状页岩的储层微观特征差异,本文以渤海湾盆地南堡凹陷古近系沙河街组一段(简称沙一段)页岩为例,综合利用氮气吸附实验、X 射线衍射(XRD)、总有机碳(TOC)、热解实验、扫描电镜实验等方法,并结合Image-J软件进行图像分析.结果表明:南堡凹陷林雀次凹沙一段页岩主要发育块状页岩和纹层状页岩,其中纹层状页岩主要发育纹层状长英质页岩、纹层状粘土质页岩和纹层状混合质页岩.纹层状页岩储集空间以微裂缝和粒间孔为主,显示有机质充填部分粒间孔,而块状页岩储集空间以粒间孔为主且有机质散状分布.纹层状页岩含油性明显好于块状页岩.纹层状页岩平均TOC为1.06%,平均S1 为1.76 mg/g;块状页岩平均TOC为0.60%,平均S1 为0.68 mg/g.储层主要发育中孔,纹层状与块状页岩储层特征存在较大差异,纹层状页岩的比表面积高于块状页岩,但孔隙度小于块状页岩.通过分析纹层与储层性质发现,随着纹层密度的增加,纹层状页岩的孔隙度增大,有机质含量减少.随着纹层厚度变异系数的增加,纹层状页岩的孔隙度减小,有机质含量增加.纹层状混合质页岩因孔隙网络复杂、连通性好、有机质丰度高,是页岩油勘探的有利岩相.

To investigate the micro-characteristics of laminated lacustrine shale,samples were collected from the first member of the Paleogene Shahejie Formation in the Nanpu Sag.An integrated approach was applied,including nitrogen adsorption,X-ray diffraction,TOC measurement,rock-eval pyrolysis,scanning electron microscopy,and image analysis using ImageJ software.The results show that the shale interval comprises both massive and laminated types,with the latter being dominated by clay,mixed,and felsic laminae.Compared to massive shale,laminated shale exhibits more developed micro-fractures,better pore connectivity,and a higher occurrence of organic matter-filled pores.In contrast,pores in massive shale are smaller and less connected,with organic matter intermittently filling only part of the intergranular pores.Geochemical analysis indicates that laminated shale has higher average TOC(1.06%)and S1 values(1.76 mg/g)than massive shale(TOC:0.60%;S1:0.68 mg/g),confirming its superior oil-bearing potential.The reservoir is dominated by medium-sized pores.While laminated shale has a larger specific surface area and average pore diameter than massive shale,its porosity is relatively lower.Furthermore,as lamina density increases,the porosity of laminated shale increases but TOC content decreases;whereas,with greater variation in grain lamina thickness,porosity decreases and TOC content increases.The laminated mixed shale is a favorable lithofacies for shale oil explora-tion due to its complex pore network,good connectivity and high organic matter abundance.

彭闻迪;刘小平;孙彪;刘国勇;王建伟;高永亮;袁瑜

油气资源与探测国家重点实验室(中国石油大学(北京)),北京 102249||中国石油大学(北京)地球科学学院,北京 102249油气资源与探测国家重点实验室(中国石油大学(北京)),北京 102249||中国石油大学(北京)地球科学学院,北京 102249油气资源与探测国家重点实验室(中国石油大学(北京)),北京 102249||中国石油大学(北京)地球科学学院,北京 102249中国石油天然气股份有限公司冀东油田分公司,河北 唐山 063004中国石油天然气股份有限公司冀东油田分公司,河北 唐山 063004中国石油天然气股份有限公司冀东油田分公司,河北 唐山 063004油气资源与探测国家重点实验室(中国石油大学(北京)),北京 102249||中国石油大学(北京)地球科学学院,北京 102249

能源科技

湖相页岩纹层孔隙结构古近系南堡凹陷渤海湾盆地

lacustrine shalelaminaepore structurePaleogeneNanpu SagBohai Bay Basin

《现代地质》 2026 (4)

1180-1196,17

国家自然科学基金项目(42072150).

10.19657/j.geoscience.1000-8527.202508240027

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