王观宏;甘华军;赵忠新;陈善斌;赵迎冬;廖佳妮;李晓宁;吴琳娜;

• 1:太原科技大学晋城校区

• 2:中国地质大学(武汉)资源学院

• 3:中国石油天然气集团公司冀东油田分公司

• 4:中海石油(中国)有限公司天津分公司渤海石油研究院

摘要(Abstract)：

根据地震数据、岩心、测井及重矿物等资料,利用EBM盆地模拟系统,模拟南堡凹陷高柳断层的活动速率和古落差,分析高柳断层活动特征及其对沉积的控制。结果表明:高柳断层的活动受南堡凹陷盆地构造演化和区域应力方向转变的联合控制,垂向上呈现"弱—强—弱"的演化趋势,平面上Es1、Ed3x、Ed3s沉积期表现明显的分段活动特征,到Ed2、Ed1和Ng沉积期,分段活动特征消失,活动均一性增强。高柳断层的活动引起南堡凹陷北部沉积中心的迁移,由拾场次凹向南迁移到高柳断层下降盘。高柳断层东段和中段连接部位、高柳断层与柏各庄断层相接部位是陆源碎屑进入凹陷的通道,高柳断层的强烈活动为扇三角洲沉积体系发育提供合适的坡降条件和可容纳空间。高柳断层对沉积体系的空间展布具有重要的控制作用,总体可划分为两种类型,即走向斜坡控砂型和断角控砂型。研究结果可为南堡凹陷构造—沉积综合分析及油气成藏预测提供参考。

关键词(KeyWords)：南堡凹陷;高柳断层;断层活动速率;分段活动性;沉积相;控砂模型

Abstract:

Keywords:

基金项目(Foundation):国家自然科学基金项目(41272122);; 国家科技重大专项(2016ZX05006-006-002)

作者(Author):王观宏;甘华军;赵忠新;陈善斌;赵迎冬;廖佳妮;李晓宁;吴琳娜;

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