含油气盆地断裂带内部结构特征及其与油气运聚的关系
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摘要
在含油气盆地中断裂对油气运移及聚集成藏起着重要的作用,本论文在断裂野外资料、岩心资料、镜下资料精细观察和描述的基础上,分析了断裂带内部结构单元发育特征,利用岩心、成像测井等资料对断裂带发育处常规测井资料进行了刻度标定,并结合定量计算法建立了综合判识断裂带及其内部结构单元的测井学方法体系。通过对断裂带内部结构影响因素的分析建立了不同地质条件下断裂带内部结构模式,并结合东营凹陷、惠民凹陷临南地区实例明确了断裂带对油气的输导、封堵机理,建立了不同类型断裂带封闭性评价方法体系,并指出了油气沿断裂走向运移方式及形成条件。结果表明:断裂带是具有复杂内部结构的三维地质体,可划分出滑动破碎带、诱导裂缝带等结构单元。滑动破碎带位于断裂中心,发育各种断层岩、伴生裂缝和断裂空腔,测井特征表现为低声波时差,低中子孔隙度,高密度,无扩径,低指示曲线值,指示曲线VU值通常在0.1~0.2以下,断裂带交会图上归一化数据范围:0.4Faults play an important role on hydrocarbon migration and accumulation in hydrocarbon-bearing basin. Based on detailed observation and description of fault outcrop, core data and microscopic flakes, this article analyzed development characteristics of fault zone internal structure units. Conventional logging data in the fault zone was calibrated by core data and imaging logging data. Then combined with quantitative calculation methods, the logging methodology was established which used to comprehensive analyze fault zone internal structure units. By factors analysis of fault zone internal structure, the model of fault zone was established in different geology conditions, then combined with examples in Dongying depression and Linnan area in Huimin depression, fault transporting and sealing mechanism was figured out, and sealing evaluation methodology of different fault types were established. Then this article pointed out that the way and conditions oil and gas migration along fault strike. The results show that fault zone is a three-dimensional geological with complex internal structure, which could be divided into sliding damage zone and induced fracture zones. Sliding damage zone is located in the center of fault zone, which developed a variety of fault rocks, associated fractures and fault cavity. And it’s logging characteristics are low acoustic time, low neutron porosity, high density, without expanding diameter, low indicative curve value, and the indicative curve VU typically less than 0.1~0.2. Normalized data of Sliding damage zone in intersection graph is 0.4
引文
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