油气藏评价与开发 ›› 2026, Vol. 16 ›› Issue (1): 153-161.doi: 10.13809/j.cnki.cn32-1825/te.2024386
杨保良1,2(
), 于雯泉1, 段宏亮1, 付茜1, 孙雅雄1,3(
), 仇永峰1, 杨艳1, 刘世丽1,3, 周进峰1, 傅强2
收稿日期:2024-09-18
发布日期:2026-01-06
出版日期:2026-01-26
通讯作者:
孙雅雄(1993—),男,博士,副研究员,从事非常规油气地质理论与评价研究。地址:江苏省扬州市文汇西路1号江苏油田分公司,邮政编码:225009。E-mail: sunyaxiong2015@163.com作者简介:杨保良(1988—),男,博士,助理研究员,从事非常规细粒沉积与页岩油气储层评价研究。地址:江苏省扬州市文汇西路1号江苏油田分公司,邮政编码:225009。E-mail: yangbl564@163.com
基金资助:
YANG Baoliang1,2(
), YU Wenquan1, DUAN Hongliang1, FU Qian1, SUN Yaxiong1,3(
), QIU Yongfeng1, YANG Yan1, LIU Shili1,3, ZHOU Jinfeng1, FU Qiang2
Received:2024-09-18
Online:2026-01-06
Published:2026-01-26
摘要:
陆相湖盆泥页岩具有岩相类型多样、垂向叠置复杂的特征,在岩相类型划分基础上开展岩相组合类型划分和有利组合优选,对于落实页岩油“甜点”层、“甜点”区具有重要意义。高邮凹陷阜宁组二段(以下简称阜二段)是苏北盆地页岩油勘探的重点区带和层系,其岩相类型单层厚度薄且纵向变化频繁,对于岩相组合类型划分及评价研究尚处于初步阶段。以高邮凹陷阜二段深层HY7井为研究对象,通过岩心观察、薄片鉴定、全岩X衍射分析、主微量元素分析等手段,在岩相类型识别和纵向沉积环境演化规律分析基础上,开展岩相组合类型划分与发育规律研究,并结合不同岩相组合类型的评价参数对比,优选有利组合类型。研究结果表明:HY7井阜二段以混积类岩相和长英质类岩相为主,以层状或纹层状长英质-灰质或白云质混积岩最为发育。阜二段沉积环境纵向上表现为气候早干晚湿、水深早浅晚深、盐度早高晚低、物源供给早高晚低、生产力早低晚高,可划分为6个演化阶段。结合各演化阶段内沉积旋回升降变化、不同岩相类型的垂向叠置关系、厚度占比等,划分出7种主要岩相组合类型。其中,层状或纹层状长英质-黏土质混积岩、长英质-灰质或白云质混积岩互层组合为最有利组合类型;层状或纹层状碳酸盐岩、长英质-灰质或白云质混积岩占主导的组合可作为较好的储集层。
中图分类号:
YANG Baoliang,YU Wenquan,DUAN Hongliang, et al. Characteristics and evaluation of lithofacies combination of fine-grained sedimentary rocks: A case study of deep second member of Funing Formation in Gaoyou Sag, Subei Basin[J]. Petroleum Reservoir Evaluation and Development, 2026, 16(1): 153-161.
表1
苏北盆地高邮凹陷阜二段岩相组合类型评价参数对比"
| 岩相组合代号 | 岩相类型 | 发育层段 | 厚度比/% | ω(TOC)/% | S1/ (mg/g) | S1+S2/ (mg/g) | 含油饱和指数/(mg/g) | 孔隙度/% | 力学脆性指数 |
|---|---|---|---|---|---|---|---|---|---|
| Ⅰ | 块状黏土质长英细粒岩、长英质-黏土质混积岩 | Ⅰ 亚段 | 11.66 | 1.58 | 0.85 | 4.59 | 54.59 | 3.71 | 30.75 |
| Ⅱ | 块状或层状长英质-灰质或白云质混积岩夹薄层长英质-黏土质混积岩 | Ⅱ、Ⅳ亚段 | 16.84 | 1.14 | 0.99 | 3.71 | 111.13 | 2.88 | 55.56 |
| Ⅲ | 层状碳酸盐岩、长英质-灰质或白云质混积岩互层 | Ⅲ亚段 | 4.90 | 0.69 | 1.07 | 2.88 | 150.43 | 3.32 | 60.84 |
| Ⅳ | 层状或纹层状的黏土质长英细粒岩或长英细砂岩、长英质-黏土质混积岩、长英质-灰质或白云质的混积岩,灰质或白云质英细粒岩互层 | Ⅴ亚段 | 14.70 | 0.51 | 0.66 | 1.46 | 121.86 | 2.57 | 45.45 |
| Ⅴ | 层状或纹层状长英质-黏土质混积岩、长英质-灰质或白云质混积岩互层 | Ⅳ亚段 | 6.92 | 1.19 | 1.01 | 4.31 | 101.54 | 4.00 | 52.60 |
| Ⅵ | 层状或纹层状长英质-灰质或白云质混积岩、灰质或白云质长英细粒岩夹薄层长英细粒岩、长英质-黏土质混积岩 | Ⅳ、Ⅴ亚段 | 30.22 | 0.70 | 1.12 | 2.35 | 140.19 | 3.01 | 54.67 |
| Ⅶ | 层状或纹层状的黏土质长英细粒岩或长英细粒岩夹薄层长英质-灰质或白云质混积岩、长英质-黏土质混积岩 | Ⅴ亚段 | 14.77 | 0.85 | 1.09 | 3.02 | 136.36 | 3.07 | 47.82 |
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