周延豪;杨少春;冯建伟;兰志勤;张博明;

• 1:中国石油大学(华东)地球科学与技术学院

• 2:山东省煤田地质规划勘察研究院

• 3:中国石油冀东油田分公司勘探开发研究院

摘要(Abstract)：

南堡凹陷古近纪断裂活动控制局部构造带的形成及沉积砂体的展布。在三维地震与测井解释基础上,采用分段评价方法,应用生长指数、古落差方法,研究南堡3号构造沙河街组沉积时期断裂活动演化特征及其控砂作用。结果表明:以沙一期为界,研究区经历两期伸展变形,分别为NW-SE与S-N向,伸展转折期为沙一下亚段,使EW向断裂逐渐增多;沙一期断裂活动强度呈现由强到弱变化趋势,不同时期区域断裂活动呈北强南弱的分区分带特征;西南部属于断裂特殊活动区域,应力状态独特,发育断裂调节带,沙一末期古地貌呈凹隆斜相间,对沉积作用具有导向意义,砂体堆积特征受地貌及断裂活动控制明显。该研究结果对类似构造带研究、南堡凹陷后续油气藏勘探具有参考意义。

关键词(KeyWords)：南堡3号构造;分段评价;断裂活动演化;两期伸展变形;断裂调节带;古地貌

Abstract:

Keywords:

基金项目(Foundation):国家自然科学基金项目(41572124)

作者(Author):周延豪;杨少春;冯建伟;兰志勤;张博明;

Email:

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