不同脆塑性演化阶段泥岩盖层内断层垂向封堵性判识方法
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本文为国家自然科学基金资助项目“断砂配置侧向分流运聚油气机理及有利部位识别研究”(编号:42072157)的成果


Identification method of fault vertical sealing in mudstone caprock at different brittle plastic evolution stages
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    摘要:

    笔者等为了研究含油气盆地不同脆塑性演化阶段泥岩盖层之上断层处油气分布特征,在不同脆塑性演化阶段泥岩盖层内断层垂向封堵机理及其影响因素研究的基础上,通过脆性演化阶段泥岩盖层古断余厚度和研究区断层在脆性泥岩盖层内分段生长上下贯通要求的最大断余厚度,判识脆性演化阶段泥岩盖层内断层垂向封堵性;通过脆塑性和塑性演化阶段断裂带内古泥岩塑性变形带连续分布指数和研究区断裂带内泥岩塑性变形带连续分布要求的最大泥岩塑性变形带连续分布指数,判识脆塑性和塑性演化阶段泥岩盖层内断层垂向封堵性,二者组合构建了一套不同脆塑性演化阶段泥岩盖层内断层垂向封堵性判识方法,用其判识渤海湾盆地黄骅拗陷歧口凹陷北部不同脆塑性演化阶段始新统沙河街组一段中亚段泥岩盖层内港东断层垂向封堵性。结果表明:沙一中亚段—东营组沉积时期脆性演化阶段沙一中亚段泥岩盖层内港东断层在测线L2903—L2213处和L2693—L2813处垂向封堵,在测线L2213—L2633处垂向不封堵,上新统明化镇组沉积时期脆塑性演化阶段沙一中亚段泥岩盖层内港东断层在测线L2093—L2273处和L2693—L2813处垂向封堵,在测线L2333—L2633处垂向不封堵,测线L2333—L2633处有利于下伏沙河街组三段源岩生成油气在渐新统东营组三段内聚集成藏,与目前港东断层处东三段已发现油气主要分布在测线L2324—L2704处相吻合,表明该方法用于判识不同脆塑性演化阶段泥岩盖层内断层垂向封堵性是可行的。

    Abstract:

    In order to study the distribution characteristics of oil and gas at faults above mudstone caprock at different brittle-plastic evolution stages in oil and gas bearing basins.Methods: Based on the study of the verticalsealing mechanism and influencing factors of faults in the mudstone cap at different brittle-plastic evolution stages, the vertical sealing of the faults in the mudstone cap in the brittle evolution stage was determined by the paleofault thickness of the mudstone cover in the brittle evolution stage and the maximum fault thickness required for the segmented growth of the fault in the brittle mudstone cover in the study area. The vertical containment of the faults in the mudstone cap at different brittle and plastic evolution stages was determined by the continuous distribution index of the paleomustone plastic deformation zone in the fault zone in the brittle plastic and plastic evolution stages and the maximum continuous distribution index of the continuous distribution of the mudstone plastic deformation zone in the fault zone in the fault zone in the study area.Results: The results show that Gangdong fault in mudstone caprock of the Middle Submember, 1st Member, Shahejie Formation(Es1Z)—Dongying Formation(Ed), Oligocene is vertically sealed at L2903—L2213 and L2693—L2813. The vertical direction of the survey line L2213—L2633 is not sealed, Gangdong fault in mudstone caprock of the Es1Z in brittle plastic evolution stage of the Minghuazhen Formation(Nm), Pliocene is sealed vertically at L2093—L2273 and L2693—L2813, but not sealed vertically at L2333—L2633, which is favorable for hydrocarbon accumulation in the Ed, Oligocene. This is consistent with the fact that oil and gas have been discovered in the 3rd Member, Dongying Formation(Ed3)of the Gangdong fault and are mainly distributed at the survey line L2324—L2704.Conclusion: The method is feasible to identify the vertical sealing properties of faults in the mudstone caprock at different brittle—plastic evolution stages.

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付广,张良伟,邓春,徐浩轩.2025.不同脆塑性演化阶段泥岩盖层内断层垂向封堵性判识方法[J].地质论评,71(6):2025060005,[DOI].
FU Guang, ZHANG Liangwei, DENG Chun, XU Haoxuan.2025. Identification method of fault vertical sealing in mudstone caprock at different brittle plastic evolution stages[J]. Geological Review,71(6):2025060005.

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  • 收稿日期:2025-04-22
  • 最后修改日期:2025-10-28
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  • 在线发布日期: 2025-11-18
  • 出版日期: 2025-11-15