松辽盆地古龙页岩有机质组成与有机质孔形成演化Organic matter compositions and organic pore evolution in Gulong shale of Songliao Basin
冯子辉,霍秋立,曾花森,王义章,贾艳双
FENG Zihui,HUO Qiuli,ZENG Huasen,WANG Yizhang,JIA Yanshuang
摘要(Abstract):
有机质孔是页岩储层重要的孔隙类型,是页岩油气富集的关键要素,其形成演化与有机质组成及生烃演化密切相关。针对古龙页岩有机质孔的发育特征及形成演化,开展地球化学分析、生排烃模拟实验、单一显微组分生烃模拟实验、微观孔隙分析等,研究古龙页岩与海相页岩有机质组成的差异,探讨古龙页岩有机质组成与有机质孔形成演化的关系。结果表明:古龙页岩有机质组成主要为层状藻类体,在不同沉积相带中比例大于50%,平均为58%,陆源高等植物来源的有机质相对较少,在深湖相区的比例平均小于10%;层状藻类体生烃转化率高,完全生烃后面积收缩率超85%,形成沿层分布的纳米级、细长条形孔(缝),是高成熟度古龙页岩孔隙的重要来源,这种孔(缝)在产状上属于黏土层间或矿物晶间孔(缝),从成因上属于有机质孔;藻类体与黏土结合的部位在有机质生烃后往往形成网状孔,孔隙骨架为残余有机质与黏土复合体。研究成果为古龙页岩成烃、成储机制研究提供重要的理论技术支撑。
As an important pore type in shale reservoirs, organic pores are critical for shale oil and gas enrichment, and their formation and evolution is closely related to organic matter compositions and hydrocarbon generation. In order to understand development characteristics, formation and evolution of organic pores in Gulong shale, organic geochemistry analyses, hydrocarbon generation pyrolysis experiments with both whole rock and individual maceral, pore characterization by FE-SEM are performed to study difference of organic matter compositions between Gulong shale and marine shale and to explore relationship between organic matter compositions and organic pore formation and evolution of Gulong shale. The results show that organic matter in Gulong shale is dominated by lamalginite with the percentage over 50% and averagly 58% in different sedimentary facies. Terrestrial organic matters are relatively less with the average percentage in deep-lake facies less than 10%.Lamalginite has higher hydrocarbon generation potential, with the surface area shrinking over 85% after complete hydrocarbon generation. The formed bedding-parallel nano-scale slender pores(fractures) are important sources for Gulong shale pores at high maturity. These pores(fractures) are clay interlayer or mineral intercrystalline pores(fractures) in occurrences, but from the view of origin, they belong to organic pores.The pores developed in transitional part between lamalginite and clay are usually spongy and the pore skeleton are the complexes of organic matter and clay. The study results provide important theoretical and technological supports for the research on hydrocarbon generating and accumulating mechanisms of Gulong shale.
关键词(KeyWords):
层状藻类体;有机质孔;热模拟实验;显微组分;古龙页岩;松辽盆地
lamalginite;organic pore;pyrolysis experiment;maceral;Gulong shale;Songliao Basin
基金项目(Foundation): 中央引导地方科技发展专项“黑龙江省致密油和泥岩油成藏研究重点实验室建设项目”(ZY20B13)
作者(Author):
冯子辉,霍秋立,曾花森,王义章,贾艳双
FENG Zihui,HUO Qiuli,ZENG Huasen,WANG Yizhang,JIA Yanshuang
DOI: 10.19597/J.ISSN.1000-3754.202107012
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- 层状藻类体
- 有机质孔
- 热模拟实验
- 显微组分
- 古龙页岩
- 松辽盆地
lamalginite - organic pore
- pyrolysis experiment
- maceral
- Gulong shale
- Songliao Basin