松辽盆地齐家凹陷南部青山口组一段基质型页岩油富集模式
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本文为国家自然科学基金项目(编号42072178、U2244207)、中国地质调查局东北地质科技创新中心区创基金项目(编号QCJJ2022- 37)和中国地质调查局地质调查项目(编号DD20230022、DD20190114)联合资助的成果


Enrichment model of tight shale oil in the first Member of Cretaceous Qingshankou Formation in the southern Qijia sag, Songliao basin
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    摘要:

    松辽盆地齐家凹陷南部白垩系青山口组一段(青一段)发育半深湖—深湖相厚层暗色泥页岩,富含典型的纯页岩基质型页岩油。以松页油1井为例,利用钻井、测录井、岩芯实验测试等资料及数据,对青一段泥页岩地质特征、岩相类型和基质型页岩油富集模式进行了研究。结果表明,青一段泥页岩存在层状、块状和纹层状3种沉积构造类型,按照“有机碳含量—沉积构造—矿物成分”三因素分类方案,可以将泥页岩划分为高有机质层状长英质泥岩、高有机质块状长英质泥岩、中有机质层状长英质泥岩、中有机质块状长英质泥岩、中有机质纹层状长英质泥岩五大岩相。其中,高有机质层状长英质泥岩相是主体岩相,也是控制页岩油富集的最有利岩相。该岩相有机质含量高(TOC值一般为2. 0%~3. 5%),含油性好(S1最大值为19. 4 mg/g),可动烃富集(可动油指数OSI平均值>300 mg/g);储集空间以介孔为主,也发育一定比例的宏孔,孔径分布较连续,主要为狭缝型孔隙,连通性较好。青一段泥页岩热演化程度较高(Ro平均值为1. 26%),有机质已大量生烃,高有机质层状长英质泥岩相原油轻质组分占比达50%~55%,流动性较好;并且发育密集层理缝,连通微纳米孔隙形成了孔缝组合网络体系,改善了泥页岩储集性能,极大提高了岩石渗流能力。总体上看,齐家凹陷南部半深湖—深湖相高有机质层状长英质泥岩相具有相对较好的页岩油富集的物质条件和有效储集空间,同时以物性致密的块状泥页岩作为顶底板隔层,页岩油保存条件好,开发潜力巨大。

    Abstract:

    Semi- deep to deep lacustrine shale strata within the first member of the Cretaceous Qingshankou Formation (K2qn1) in the southern Qijia sag of the Songliao basin are well- developed and represent a typical target for tight shale oil exploration. Using data from drilling, logging, and core tests, we conducted a comprehensive study of the geological characteristics, lithofacies type, and tight shale oil enrichment model of the K2qn1 using the SYY1 well as an example. Our results indicate the K2qn1 shale exhibits three kinds of sedimentary structures: Bedded, massive, and laminated. Based on total organic matter (TOC) content, sedimentary structure, and mineral composition, the K2qn1 shale in the SYY1 well can be divided into five lithofacies: Bedded siliceous mudstone with high TOC (>2. 0%), massive siliceous mudstone with high TOC, bedded siliceous mudstone with moderate TOC (1. 0%~2. 0%), massive siliceous mudstone with moderate TOC, and laminated siliceous mudstone with moderate TOC. Among these, the bedded siliceous mudstone lithofacies with high TOC is the main lithofacies and the most favorable to control the enrichment of shale oil. It boasts high organic matter content (TOC values generally ranging from 2% to 3. 5%), good free oil content (S1 values up to 19.4 mg/g), and abundant movable hydrocarbons (average OSI values exceeding 300 mg/g). Its reservoir space is mainly mesoporous, with a proportion of macropores also developed. Compared to other lithofacies, it exhibits a relatively continuous pore size distribution, dominated by slit pores, and good connectivity. The K2qn1 shale in the SYY1 well displays a high thermal evolution degree (average Ro value of 1. 26%), indicating significant hydrocarbon generation from organic matter. In the bedded siliceous mudstone lithofacies with high TOC, light components constitute 50% to 55% of the shale oil, implying good oil mobility. In addition, this lithofacies is characterized by well- developed, dense bedding fractures. These fractures connect micro- nano pores, forming a pore- fracture network system that significantly enhances reservoir performance and rock permeability. Therefore, the bedded siliceous mudstone lithofacies with high TOC, developed in the semi- deep to deep lacustrine facies of the southern Qijia sag, presents a promising target for shale oil exploration. This lithofacies exhibits favorable material conditions and effective reservoir space for shale oil enrichment, while the surrounding tight massive shale acts as an effective seal, ensuring excellent preservation conditions.

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姚玉来,肖飞,李士超,杨建国,黄一鸣,叶春林.2024.松辽盆地齐家凹陷南部青山口组一段基质型页岩油富集模式[J].地质学报,98(11):3393-3407.
YAO Yulai, XIAO Fei, LI Shichao, YANG Jianguo, HUANG Yiming, YE Chunlin.2024. Enrichment model of tight shale oil in the first Member of Cretaceous Qingshankou Formation in the southern Qijia sag, Songliao basin[J]. Acta Geologica Sinica,98(11):3393-3407.

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  • 收稿日期:2024-08-19
  • 最后修改日期:2024-08-19
  • 录用日期:2024-08-19
  • 在线发布日期: 2024-09-27