首页|海陆相页岩孔隙结构对比研究——以龙马溪组和芦草沟组为例

海陆相页岩孔隙结构对比研究——以龙马溪组和芦草沟组为例

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不同沉积背景下形成的页岩,其孔隙结构存在差异.以湘西北地区龙马溪组海相页岩和新疆吉木萨尔凹陷芦草沟组陆相页岩为研究对象,通过元素地球化学分析、矿物学分析、气体吸附实验及高压压汞实验等定量方法与场发射扫描电镜观察的定性方法相结合,明确了不同沉积背景下页岩的孔隙结构差异,结合沉积环境的研究揭示了研究区海相页岩和陆相页岩孔隙结构差异的控制因素.结果表明:龙马溪组海相页岩发育大量有机孔,孔径主要分布在微孔和中孔范围内;芦草沟组陆相页岩有机孔发育较少,分布在中孔-宏孔尺度的无机孔则是孔隙系统的主要贡献者.龙马溪组海相页岩具有较高的初级生产力及良好的底水保存条件,有机质成熟度较高,有机质丰度是控制孔隙发育的主要因素;而芦草沟组陆相页岩尽管在缺氧环境及较高的生产力条件下沉积,有机质含量高,但成熟度低,有机孔发育有限,黏土矿物含量是控制孔隙发育的主要因素.通过研究海相与陆相页岩孔隙结构的差异及主控因素,以期为研究区后续的页岩油气勘探开发工作提供理论依据.
Comparative study on pore structure of marine and terrestrial shales:A case study of Longmaxi Formation and Lucaogou Formation
The pore structures of shale formed under different sedimentary backgrounds are different.Taking the marine shale of Longmaxi Formation in Northwest Hunan Province and the terrestrial shale of Lucaogou Formation in Jimushar Depression,Xinjiang Province,were taken as the objects of study,and the quantitative methods such as elemental geochemical analysis,mineralogical analysis,gas adsorption experiment,high-pressure mercury intrusion experiment,and the qualitative methods such as field emission scanning electron microscopy observation were combined.Then,the differences in the pore structures of shales in different depositional backgrounds were clearly defined,and the controlling factors for the differences in pore structures between the marine and terrestrial shales in the study area were revealed in combination with the study of the depositional environments.The results show that Longmaxi Formation marine shale develops a large number of organic pores,and the pore sizes range from micropores to mesopores;the organic pores of the terrestrial shale of Lucaogou Formation are less developed,and the inorganic pores distributed in the mesopore-macroporous scale are the main contributors to the pore system.The marine shales of Longmaxi Formation have high primary productivity and good bottom water preservation conditions,with high organic matter maturity,and the organic matter abundance is the main factor controlling pore development;.However,the terrestrial shales of Lucaogou Formation deposit in anoxic environments and have high productivity conditions,with a high organic matter content but a low maturity and limited development of organic pores.The clay mineral content is the main factor controlling the development of pore space.By studying the differences in pore structures between marine and terrestrial shales and the main controlling factors,we hope to provide a theoretical basis for the subsequent shale oil and gas exploration and development work in the study area.

Longmaxi Formationshale reservoirspore structure

刘文慧、马啸、户瑞宁、吴胡日查、谭静强、骆若冰

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中南大学地球科学与信息物理学院,长沙 410083

地球化学过程与资源环境效应湖南省重点实验室,长沙 410116

龙马溪组 页岩储层 孔隙结构

国家自然科学基金湖南省科技计划

U23B201552023RC1021

2024

非常规油气

非常规油气

ISSN:
年,卷(期):2024.11(3)
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