石油与天然气地质 ›› 2025, Vol. 46 ›› Issue (2): 392-406.doi: 10.11743/ogg20250205
李军亮1(
), 王民2,3(
), 秦峰1, 王勇1, 魏晓亮1, 孟伟1, 沈安超2,3, 宋兆京2,3, 余昌琦2,3, 李俊乾2,3, 刘嘉祺2,3
收稿日期:2024-11-26
修回日期:2025-03-07
出版日期:2025-04-30
发布日期:2025-04-27
通讯作者:
王民
E-mail:lijunliang.slyt@sinopec.com;wangm@upc.edu.cn
第一作者简介:李军亮(1975—),男,博士、高级工程师,油气地质综合研究。E-mail: lijunliang.slyt@sinopec.com。
基金项目:
Junliang LI1(
), Min WANG2,3(
), Feng QIN1, Yong WANG1, Xiaoliang WEI1, Wei MENG1, Anchao SHEN2,3, Zhaojing SONG2,3, Changqi YU2,3, Junqian LI2,3, Jiaqi LIU2,3
Received:2024-11-26
Revised:2025-03-07
Online:2025-04-30
Published:2025-04-27
Contact:
Min WANG
E-mail:lijunliang.slyt@sinopec.com;wangm@upc.edu.cn
摘要:
陆相页岩油勘探已取得突破,但页岩油富集高产的主控地质因素尚不清晰,制约着页岩油的高效开发。精细刻画不同纹层特征可揭示页岩油富集主控因素。本文以济阳坳陷古近系沙河街组富碳酸盐页岩为研究对象,通过薄片鉴定和场发射扫描电镜观察,剖析了典型纹层储集空间和含油性的特征,揭示了页岩纹层组合对页岩油富集的控制作用。研究发现,济阳坳陷沙河街组四段上亚段富碳酸盐页岩的纹层可划分为纤维状方解石纹层、泥晶方解石纹层、粉晶方解石纹层、富黏土矿物纹层和混合矿物纹层5种类型,主要发育“泥晶方解石纹层+富黏土矿物纹层+混合矿物纹层”和“纤维状方解石纹层+粉晶方解石纹层+富黏土矿物纹层+混合矿物纹层”2种纹层组合模式;富黏土矿物纹层和混合矿物纹层有机质含量高,是页岩油富集的物质基础;粉晶方解石纹层储集空间发育,是页岩油储集的优势纹层;富黏土矿物纹层与粉晶方解石纹层或泥晶方解石纹层叠置分布,可构成页岩油富集的最佳纹层配置,该类纹层组合的富碳酸盐页岩是页岩油勘探开发的重要目标。
中图分类号:
图3
济阳坳陷樊斜184井沙四上亚段页岩泥晶方解石纹层产状特征显微照片a.泥晶方解石纹层与富黏土矿物纹层的互层,泥晶方解石纹层呈灰黄色,与黏土层渐变接触,埋深3 550.35 m,单偏光,普通薄片;b.透镜状泥晶方解石顺层发育在泥质纹层中,埋深3 550.35 m,单偏光,普通薄片;c.堆积发育的泥晶方解石透镜体,埋深3 568.85 m,单偏光,普通薄片;d.泥晶方解石透镜体与脉体混合发育,埋深3 550.35 m,单偏光,普通薄片;e.泥晶方解石透镜体发育在富黏土矿物纹层中,层内可见较多的生物碎屑,埋深3 568.85 m,单偏光,普通薄片;f.泥晶方解石矿物组成特征,埋深3 550.35 m,扫描电镜(Cal为方解石,Qz为石英)"
图5
济阳坳陷樊斜184井沙四上亚段页岩富黏土矿物纹层产状特征显微照片a.较纯的富黏土矿物纹层,含碎屑颗粒少,纹层表面平整,埋深3 529.34 m,单偏光,普通薄片;b.含透镜体的富黏土矿物纹层,透镜体顺层发育,埋深3 529.34 m,单偏光,普通薄片;c.富黏土矿物纹层矿物组成特征,大量有机质充填,埋深3 529.34 m,扫描电镜(Cal为方解石,Qz为石英,Dol为白云石,Py为黄铁矿,Clay为黏土矿物);d.与泥晶方解石脉互层的富黏土矿物纹层,埋深3 358.20 m,单偏光,普通薄片;e.富黏土矿物纹层中发育大量的层状藻,埋深3 358.20 m,荧光(与d图同视域),普通薄片;f.碎屑颗粒含量较高的泥质层,受有机质含量影响,颜色较纯泥质层变淡,埋深3 358.20 m,单偏光,普通薄片"
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