石油与天然气地质 ›› 2020, Vol. 41 ›› Issue (6): 1151-1161.doi: 10.11743/ogg20200604

• 油气地质 • 上一篇    下一篇

苏北盆地黄桥地区富CO2流体对油气储-盖系统的改造作用

周冰1,2(), 金之钧1,2, 刘全有1,2, 伦增珉1,2, 孟庆强1,2, 朱东亚1,2   

  1. 1. 中国石化 石油勘探开发研究院, 北京 100083
    2. 页岩油气富集机理与有效开发国家重点实验室, 北京 100083
  • 收稿日期:2018-08-20 出版日期:2020-12-28 发布日期:2020-12-09
  • 第一作者简介:周冰(1988-),女,博士、副研究员,含油气盆地中流体-岩石相互作用。E-mail:zhoubing.syky@sinopec.com
  • 基金项目:
    国家重点研发计划项目(2016YFB0600804);国家自然科学基金青年基金项目(41602160)

Alteration of reservoir-caprock systems by using CO2-rich fluid in the Huangqiao area, North Jiangsu Basin

Bing Zhou1,2(), Zhijun Jin1,2, Quanyou Liu1,2, Zengmin Lun1,2, Qingqiang Meng1,2, Dongya Zhu1,2   

  1. 1. Petroleum Exploration and Production Research Institute, SINOPEC, Beijing 100083, China
    2. State Key Laboratory of Shale Oil and Gas Enrichment Mechanisms and Effective Development, Beijing 100083, China
  • Received:2018-08-20 Online:2020-12-28 Published:2020-12-09

摘要:

查明富CO2流体对储-盖系统的改造作用,对于研究CO2活动与油气成藏效应、CO2储存和CO2驱油提高采收率有着重要意义。选取下扬子苏北盆地黄桥地区和句容地区的二叠系龙潭组储层和大隆组盖层组合,分别作为有无CO2流体活动的对比研究对象。通过薄片观察统计、矿物成分和碳同位素分析,查明了两个地区储层的异同点。黄桥地区储层的自生矿物以石英次生加大边和高岭石充填为主,发育少量片钠铝石,句容地区不发育片钠铝石,且次生石英含量不高;黄桥地区储层孔隙度明显高于句容地区,薄片下观察到大量长石溶蚀孔隙,偶见长石溶蚀孔内生长片钠铝石雏晶,是CO2与长石发生水岩相互作用的直接证据;黄桥地区和句容地区盖层均为黑色块状泥岩,黄桥地区盖层发育微裂隙,但裂隙均已再充填方解石脉,碳同位素数据表明方解石脉为富CO2流体活动结果,在句容地区泥岩盖层中未见大量裂隙和矿物脉。综合研究分析表明,富CO2流体充注引起储层砂岩中长石大量溶蚀,增加了孔隙空间,片钠铝石、次生石英和高岭石自生矿物组合序列沉淀,同时富CO2流体的连续活动导致泥岩盖层发生方解石沉淀,充填盖层裂缝,有利于提高盖层的封盖能力。

关键词: 改造作用, 相互作用, 封盖能力, 储-盖系统, 富CO2流体, 黄桥地区, 苏北盆地

Abstract:

The mechanisms of CO2-rich fluid in the alteration of reservoir-caprock systems are worthy of study for understanding the links between hydrocarbon accumulation and CO2 activities, exploring the possibility of geological storage of CO2 and improving the effectiveness of enhanced oil recovery (EOR) with CO2 flooding.This study is focused on a comparison of reservoir-caprock systems with and without CO2 fluid activities in the Longtan and Dalong Formations of the Permian in the Huangqiao and Jurong areas, North Jiangsu Basin, Lower Yangtze region.The results based on thin sections observation, mineral composition and carbon isotope analyses of the areas show that the authigenic minerals in the reservoirs of the Huangqiao area are dominated by secondary overgrowth of quartz and kaolinite, followed by a small amount of dawsonite, whereas those in the Jurong area contain no dawsonite at all and have only limited amount of secondary quartz.The reservoir porosity of the Huangqiao area is markedly higher than that of the Jurong area.Thin section observation reveals a large number of dissolved pores in feldspar occasionally with dawsonite in samples from the Huangqiao area—a piece of direct evidence of interaction between CO2 and feldspar.Both caprocks in the two areas are black blocky mudstones.There are micro-cracks refilled with calcite veins in the caprocks of the Huangqiao area.And carbon isotope data show that the calcite veins are the result of CO2-rich fluid activities.While few cracks and mineral veins are discovered in the mudstone caprocks from the Jurong area.These results indicate that the charging of CO2-rich fluid in the reservoirs caused large-scale dissolution of feldspar, which increased pore space and precipitation of typical authigenic mineral assemblages of dawsonite, secondary quartz and kaolinite.The continuous activities of the CO2-rich fluid led to precipitation of calcite and subsequent filling-up of cracks and pores in the caprocks, thus providing a better sealing effect.

Key words: alteration, interaction, sealing capacity, reservoir-caprock system, CO2-rich fluid, Huangqiao area, North Jiangsu Basin

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