首页|盐构造活动对油气成藏的控制作用:以下刚果盆地为例

盐构造活动对油气成藏的控制作用:以下刚果盆地为例

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盐构造对油气藏成藏具有重要的控制作用,很多富油气盆地都发育丰富的盐构造.本论文以南大西洋东海岸下刚果盆地为研究对象,从含油气盆地分析的角度,以构造地质学、沉积学和成藏动力学系统理论为指导,旨在明确盐岩构造变形特征及演化过程的基础上,分析盐岩构造变形对盐相关油气成藏的控制作用.基于二维和三维地震资料解释成果,识别出下刚果盆地发育盐滚、盐底辟、盐蓬/盐盖、厚层盐岩4种主要盐岩构造样式,明确了各类盐构造的变形特征及其上覆地层构造特征.最后,在分析盐构造变形对源、储、圈闭等静态成藏要素,以及圈闭演化过程、油气运移、保存等动态成藏过程影响的基础上,建立下刚果盆地油气动态成藏模式,以期指导该盆地下一步油气勘探.
Salt tectonic activity controlling on hydrocarbon accumulation:A case of the Lower Congo Basin
Salt structure plays an important role in controlling the hydrocarbon accumulation,and many oil-rich basins are rich in salt structure.From the perspective of petroliferaceous basin analysis,taking the Lower Congo Basin in the east coast of the South Atlantic Ocean as the research object,based on the theory of structural geology,sedimentology and hydrocarbon accumulation dynamic,the paper aims to analyze the control effect of salt structure deformation on salt-related oil and gas accumulation,on the basis of the deformation characteristics and evolution process of salt structure.Based on the interpretation of 2D and 3D seismic data,four major salt structures,including salt roller,diapiric salt,canopy salt and missive salt,were identified in the Lower Congo Basin,and the deformation characteristics of various salt structures and the tectonic characteristics of their overlying strata were defined.Finally,based on the analysis of the influence of salt tectonic deformation on the static factors for hydrocarbon accumulation such as source,reservoir and trap,and the dynamic processes for hydrocarbon accumulation such as the evolution of trap,hydrocarbon migration and preservation,the dynamic hydrocarbon accumulation model of the Lower Congo Basin was established,aiming to guide the future oil and gas exploration in this basin.

Lower Congo BasinSalt structureProcess of hydrocarbon accumulationModel of hydrocarbon accumulation

刘静静、邬长武、郭荣涛、高蔚原、汲生珍、李晋

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中国石化石油勘探开发研究院 北京 100083

中联煤层气国家工程研究中心 北京 100095

下刚果盆地 盐构造 成藏过程 成藏模式

国家科技重大专项中国石化科技部项目

2016ZX05033001-003P21043-4

2024

地质科学
中国科学院地质与地球物理研究所

地质科学

CSTPCD北大核心
影响因子:0.79
ISSN:0563-5020
年,卷(期):2024.59(2)
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