新疆石油地质 ›› 2024, Vol. 45 ›› Issue (3): 286-295.doi: 10.7657/XJPG20240305

• 油气勘探 • 上一篇    下一篇

玛湖凹陷风城组储集层孔喉结构及流体赋存特征

朱越(), 伍顺伟, 邓玉森, 刘林, 雷祥辉, 牛有牧   

  1. 中国石油 新疆油田分公司 勘探开发研究院,新疆 克拉玛依 834000
  • 收稿日期:2024-02-05 修回日期:2024-03-11 出版日期:2024-06-01 发布日期:2024-05-23
  • 作者简介:朱越(1989-),女,湖北潜江人,工程师,硕士,石油地质,(Tel)0990-6880321(Email)zhuyue66@petrochina.com.cn
  • 基金资助:
    中国石油攻关性应用性科技专项(2023ZZ15)

Pore Throat Structures and Fluid Occurrences of Reservoirs in Fengcheng Formation, Mahu Sag

ZHU Yue(), WU Shunwei, DENG Yusen, LIU Lin, LEI Xianghui, NIU Youmu   

  1. Research Institute of Exploration and Development, Xinjiang Oilfield Company, PetroChina, Karamay, Xinjiang 834000, China
  • Received:2024-02-05 Revised:2024-03-11 Online:2024-06-01 Published:2024-05-23

摘要:

为了揭示和对比玛湖凹陷北部风城组砂岩和泥页岩2类岩性储集层微观结构及不同尺寸孔隙内流体赋存特征,基于高压压汞、核磁共振、大视域拼接电镜扫描等实验,定量表征2类岩性储集层的孔喉尺寸和流体赋存特征,并对比原始样品和加压饱和原油样品的核磁共振以及抽提前后的高压压汞实验结果,揭示不同尺寸孔喉系统内束缚态流体和可动流体的分布。研究表明:2类岩性储集层孔隙和喉道尺寸差异均不明显,主要发育直径为0.01~10.00 μm的孔隙和半径小于10.00 nm的喉道,以中孔-细喉为主,其中,泥页岩孔隙直径略大于砂岩,喉道半径略小于砂岩。泥页岩多发育晶间孔、蜂窝状溶孔等导管状孔,砂岩导管状孔和球形孔各占一半,且随着孔径增大,粒间孔、粒间溶孔等球形孔占比增大。流体赋存及可动性受矿物组分、孔径等多种因素影响,有机质、白云石以及黄铁矿的偏油润湿性以及黏土矿物晶间孔的强毛细管束缚致使页岩油可动性降低,可动流体主要分布在直径大于300 nm的中—大孔隙内。综合储集层物性和可动流体分布特征,研究区页岩油有利区块为东部的玛51X井区,该井区泥页岩和砂岩均可作为有利的开发对象。

关键词: 玛湖凹陷, 风城组, 储集层, 页岩油, 孔喉结构, 流体赋存

Abstract:

In order to reveal and compare the microstructures of sandstone and shale reservoirs, and the fluid occurrences within different sizes of pores in the Fengcheng formation of the Mahu sag, the experiments including high-pressure mercury intrusion (HPMI), nuclear magnetic resonance (NMR), and large-view splicing SEM were conducted to quantitatively characterize the pore throat size and fluid occurrence characteristics of the two types of reservoirs. The NMR experimental results and the HPMI experimental results before and after extraction of the original samples and the pressurized oil-saturated sample were compared to reveal the distributions of bound and movable fluids within pores of different sizes. The results indicate that sandstone and shale do not differ significantly in the sizes of pores and throats, which are dominantly 0.01-10.00 μm in pore diameter and <10.00 nm in throat radius, respectively, indicative of mesopores and fine throats. Shale has slightly larger pore diameters but smaller throat radii than sandstone. Shale mainly develops tubular pores such as intercrystalline pores and honeycomb-like dissolution pores. Sandstone has an equal distribution of tubular and spherical pores, with the proportion of spherical pores such as intergranular pores and intergranular dissolution pores increasing as the pore size increases. Fluid occurrence and mobility are controlled by multiple factors such as mineral composition and pore size. The oil-wet properties of organic matter, dolomite and pyrite, and the strong capillary confinement of intergranular pores in clay minerals, reduce the mobility of shale oil, and the movable fluids are mainly distributed in mesopores-macropores with diameters greater than 300 nm. Combining the reservoir physical properties and movable fluid distribution, it is determined that the favorable shale oil block in the study area is the Ma 51X well block, both shale and sandstone in the well block are favorable targets for development.

Key words: Mahu sag, Fengcheng formation, reservoir, shale oil, pore throat structure, fluid occurrence

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