西南石油大学学报(自然科学版) ›› 2025, Vol. 47 ›› Issue (6): 37-46.DOI: 10.11885/j.issn.1674-5086.2024.09.12.01

• 地质勘探 • 上一篇    下一篇

宝岛A深水大气田低渗储层成岩作用及孔隙演化研究

杨丽, 李华, 王攀荣, 彭志春, 潘燕   

  1. 中海石油(中国)有限公司海南分公司, 海南 海口 570311
  • 收稿日期:2024-09-12 发布日期:2026-01-12
  • 通讯作者: 杨丽,E-mail:agoodheaven@163.com

Diagenesis and Pore Evolution in Low-permeability Reservoirs of the Baodao A Deepwater Gas Field

YANG Li, LI Hua, WANG Panrong, PENG Zhichun, PAN Yan   

  1. Hainan Branch CNOOC China Limited, Haikou, Hainan 570311, China
  • Received:2024-09-12 Published:2026-01-12

摘要: 宝岛A 气田是在宝岛凹陷发现的首个深水、深层大气田。宝岛A 气田的主力气组为陵水组三段,该气田水深变化大,断裂系统发育,储层非均质性强,埋深大,成岩作用普遍发育,受成岩作用改造的影响,储层物性差且分布规律复杂。为此,根据岩石薄片和黏土矿物X 衍射等分析化验资料,详细描述了研究区陵水组三段深水深层低渗储层的岩石物性特征、成岩特征、成岩序列及孔隙定量演化等。研究表明,机械压实作用降低孔隙度约22.0%,是宝岛A 气田陵水组三段储层致密的最主要因素。溶解作用增加了储层孔隙度约11.9%,胶结作用使储层孔隙度降低了13.7%。孔隙演化过程揭示,压实作用是早期储层物性变差的主要因素,中晚期油气充注,使矿物溶蚀改善了储集空间,晚期碳酸盐胶结进一步使储层致密。该研究成果有效指导优势储层预测研究,为气田高效开发提供地质依据,为保障国家加快进军深海步伐奠定基础。

关键词: 成岩作用, 孔隙演化, 低渗储层, 成岩序列, 深水气田

Abstract: Baodao A Gas Field is the first deep water and deep gas field discovered in Baodao Depression. The main gas group of the Baodao A Gas Field is the third member of the Lingshui Formation. The water depth of the gas field varies greatly, the fault system is well developed, the reservoir highly heterogeneous, and the diagenetic phenomena abundant. Affected by the diagenetic transformation, the physical properties of the gas field are poor and the distribution law is complex. Therefore, based on the experimental data of thin section of rock, X-ray diffraction of clay minerals, and oxygen isotope analysis, the reservoir physical property, diagenetic characteristics and quantitative evolution of pores of the low permeability reservoir in the third member of Lingshui Formation in the study area are systematically described. The results show that: mechanical compaction reduces the porosity of the reservoir by 22.0%, which is the main factor of reservoir compaction in the third member of Lingshui Formation in the study area. The porosity of the reservoir is increased by 11.9% by solution and decreased by 13.7% by cementation. The process of pore evolution reveals that compaction is the primary factor contributing to early changes in reservoir physical properties, while mineral dissolution during the middle and late stages of oil and gas charging enhances reservoir space. Subsequently, late-stage carbonate cementation further densifies the reservoir. This research achievement effectively guides the prediction research of favorable reservoirs, provides geological basis for the efficient development of gas fields, and lays a foundation for ensuring the country’s accelerated advancement into the deep sea.

Key words: diagenesis, pore evolution, low permeability reservoir, diagenetic sequence, deepwater gas field

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