苏北盆地阜二段页岩油保存条件对比分析
Comparative analysis of preservation conditions for shale oil in second member of Funing Formation, Subei Basin
- 2026年16卷第2期 页码:274-285
收稿:2024-09-10,
纸质出版:2026-03-26
DOI: 10.13809/j.cnki.cn32-1825/te.2024352
移动端阅览
收稿:2024-09-10,
纸质出版:2026-03-26
移动端阅览
苏北盆地溱潼、高邮、金湖和海安凹陷古近系阜宁组二段(阜二段)页岩油勘探相继取得突破,是下一步增储上产的重要领域。各主力凹陷阜二段页岩油成藏演化过程差异较大,页岩油保存条件的差异性、控制因素和地层超压的发育规律认识不清,制约了下一步勘探部署。从主力凹陷差异演化过程研究入手,结合顶底板条件、断层发育及活动性对比分析,明确了各凹陷页岩油保存条件差异性及影响因素,并揭示了复杂断块区异常高压的保存机制。结果表明,盆地东西部阜二段底板沉积相带的差异性是形成现今地层超压差异的基础;吴堡事件各凹陷内断层的活动性和发育程度,以及盆地西侧郯庐断裂带活动性对盆地各凹陷的差异控制作用(从西往东,各凹陷阜二段断层晚期活动性逐渐减弱),是各凹陷现今地层超压差异的核心;盐城组沉积中晚期,盆地东部的海安、盐城凹陷初次进入生烃门限,而中西部的溱潼、高邮和金湖凹陷局部经历加深、加熟和再次生烃,是各凹陷现今地层超压差异的关键。中—高成熟度页岩油首选勘探有利区位于金湖、高邮、溱潼凹陷的深凹稳定区,中—低成熟度页岩油首选勘探有利区位于海安和盐城凹陷的深凹区。此外,凹陷内部,断层规模越大,距离断层越近越不利于页岩油保存。研究成果对陆相断陷盆地页岩油勘探具有指导意义。
Exploration breakthroughs of shale oil have been successively achieved in the second member of the Paleogene Funing Formation in four main sags (Qintong
Gaoyou
Jinhu
and Haian) of the Subei Basin
marking an important area for future increases in reserves and production. The evolution of shale oil accumulation processes differs greatly among major sags. The unclear understanding of the differences in preservation conditions
controlling factors
and the development patterns of formation overpressure for shale oil has constrained further exploration deployment. Starting from the differential evolution processes of the major sags
and combined with a comparative analysis of the top-bottom conditions
fault development
and fault activity
the differences in shale oil preservation conditions and their influencing factors across various sags were clarified. Additionally
the preservation mechanisms of abnormal overpressure in complex fault-block areas was revealed. The results indicated that the differences in the sedimentary facies belts of the second member of the Paleogene Funing Formation’s base in the eastern and western parts of the basin formed the basis for current differences in formation overpressure. The activity and development degree of faults within each sag during the Wubao event
as well as the differential controlling effect of the Tan-Lu fault zone on the western part of the basin on each sag (manifested as a gradual weakening of late-stage fault activity in the second member of the Paleogene Funing Formation from west to east)
constituted the core of current differences in formation overpressure across the sags. During the middle to late stage of sedimentation of the Yancheng Formation
the Haian and Yancheng Sags in the eastern part of the basin first entered the hydrocarbon generation threshold
while the Qintong
Gaoyou
and Jinhu Sags in the central and western part experienced local deepening
increased thermal maturity
and secondary hydrocarbon generation. This process was crucial in the current differences in formation overpressure across the sags. For medium-to-high maturity shale oil
the preferred favorable exploration areas were located in the deep and stable zones of the Jinhu
Gaoyou
and Qintong Sags. For low to medium maturity shale oil
the preferred favorable exploration areas were located in the deep zones of the Haian and Yancheng Sags. Moreover
within a sag
larger fault scales and closer proximity to faults were less favorable for shale oil preservation. The research findings provide guidance for shale oil exploration in continental fault-depression basins.
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