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琼东南盆地陵水凹陷LS13-2区断裂特征及控藏作用OA

Fault characteristics and their control on accumulation in block LS13-2 of Lingshui Sag,Qiongdongnan Basin

中文摘要英文摘要

陵水凹陷 LS13-2 区是琼东南盆地北部梅山组唯一具有自然产能的探区,其成藏组合属于"下生上储"类型.通源断裂作为沟通烃源岩与储层的"桥梁",在油气垂向运移和成藏过程中起着关键作用.为明确该区的断裂特征及其对油气成藏的控制机制,以 F2、Fs 及古构造脊上方花状断裂为主要研究对象,基于张扭断裂相关褶皱理论与精细构造解析技术,系统分析了断裂的样式、级别、期次、活动强度、演化模式及形成机制,并结合已钻井生产资料对断裂的输导性与封闭性等控藏作用进行了综合评价.LS13-2 区发育"三类、三级、三期"断裂体系,F2、Fs 和古构造脊上方花状断裂分别属于二级、三级和四级断裂,分别在断陷期、乐东组及三亚组沉积期活动.构造演化可划分为早始新世、渐新世、早中新世和上新世 4 期构造运动,断裂的形成机制受古构造脊等先存构造控制明显.区内断裂可分为持续输导型、晚期输导型和复合输导型 3 种类型,其中 F2 持续输导型断裂及 Fs 晚期输导型断裂的西部构成了有利输导体系.在封闭性方面,梅山组砂体发育,F2 断裂中段封闭性较好,西段与东段较差;而三亚组整体呈"泥包砂"组合,封闭性显著优于梅山组.具备梅山组有利保存条件与三亚组规模储层发育的圈闭,有望成为研究区下一步油气勘探的有利目标.

In the northern part of the Qiongdongnan Basin,the block LS13-2 of the Lingshui Sag is the only explo-ration area in the Meishan Formation known to have natural productivity,representing an accumulation model of source in the lower section and reservoir in the upper section.Source-connected faults serve as a bridge connecting source rocks and reservoirs,playing an important role in the vertical migration and accumulation of oil and gas.To clarify the fault characteristics and their controlling mechanisms on oil and gas accumulation in this area,the study focused on the F2,Fs,and flower-shaped faults above the paleotectonic ridge.The fault patterns,levels,periods,activity intensity,evolution models,and formation mechanisms were systematically analyzed based on the transtensional fault-related fold theory and detailed structural interpretation techniques.The accumulation controlling effects of faults through oil and gas transport and sealing were comprehensively evaluated in combina-tion with production data from drilled wells.The block LS13-2A developed a fault system of three types,three grades,and three periods.The F2,Fs,and flower-shaped faults above the paleotectonic ridge were classified as second-,third-,and fourth-level faults,which were active during the fault-depression period,the Ledong Forma-tion and the Sanya Formation sedimentary periods,respectively.Tectonic evolution were divided into four stages:Early Eocene,Oligocene,Early Miocene,and Pliocene.The formation mechanisms of the faults were obviously controlled by paleo-tectonic ridges and other preexisting structures.Faults in the area were divided into three types:continuous transport,late transport,and composite transport.Among them,the continuous transport F2 fault and the western part of the late transport Fs fault constituted a favorable transport system.Regarding sealing capacity,sand bodies were well developed in the Meishan Formation.The sealing capacity of the middle section of the F2 fault was relatively good,while the western and eastern sections were poor.In contrast,the Sanya For-mation overall showed a mudstone-encased sandstone assemblage,and its sealing capacity was significantly better than that of the Meishan Formation.Traps which possess favorable preservation conditions in the Meishan Forma-tion and large-scale reservoir development in the Sanya Formation are expected to become favorable targets for the next step of oil and gas exploration in the study area.

张驰;周雨双;杨鹏程;王旖旎;姚威;路清华;孔令文

中国石化 石油勘探开发研究院 无锡石油地质研究所,江苏 无锡 214126中国石化 石油勘探开发研究院 无锡石油地质研究所,江苏 无锡 214126中国石化 上海海洋油气分公司 勘探开发研究院,上海 200120中国石化 上海海洋油气分公司 勘探开发研究院,上海 200120中国石化 石油勘探开发研究院 无锡石油地质研究所,江苏 无锡 214126中国石化 石油勘探开发研究院 无锡石油地质研究所,江苏 无锡 214126中国石化 石油勘探开发研究院 无锡石油地质研究所,江苏 无锡 214126

能源科技

断裂特征成因机制断裂输导性断裂封闭性陵水凹陷LS13-2区琼东南盆地

fault characteristicsgenesis mechanismfault transportfault sealingblock LS13-2 in the Ling-shui SagQiongdongnan Basin

《石油实验地质》 2026 (2)

409-417,9

中国石化科技部项目(P23134、P24180)资助.

10.11781/sysydz2026020409

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