岩性油气藏 ›› 2024, Vol. 36 ›› Issue (3): 106116.doi: 10.12108/yxyqc.20240310
董柔1,2, 李坤2, 殷际航2, 薛煜恒2, 江涛3, 徐国盛2
DONG Rou1,2, LI Kun2, YIN Jihang2, XUE Yuheng2, JIANG Tao3, XU Guosheng2
摘要: 以三维地震精细解释为基础,通过构造剖面恢复,系统分析了渤东凹陷新生代伸展-走滑叠合断裂的时空差异演化特征及控藏作用。研究结果表明:①渤东凹陷新生代广泛发育以 NNE 向为主干、NE向为派生、NW 向为叠加的伸展-走滑叠合断裂体系,可划分为强伸展-弱走滑断裂和强走滑-弱伸展断裂 2 类;整体具有深浅分层、南北分段的特征,纵向上,古近系主要发育强伸展-弱走滑断裂,断裂大而稀,新近系—第四系主要发育强走滑-弱伸展断裂,断裂小而密;平面上,同一断裂在不同段的构造组合样式存在差异。②研究区新生代伸展-走滑叠合断裂的演化主要表现为北部断裂活动强度“早强晚弱”,中部断裂继承性持续发育,南部断裂活动强度“早弱晚强”;演化模式分为初始断陷(孔店组—沙四段沉积期)、强烈断陷(沙三段—东营组沉积期)和走滑坳陷(馆陶组—平原组沉积期)3 个阶段,初始断陷阶段,NNE—NE 向强伸展与弱走滑叠合,NE 向强伸展-弱走滑断裂为主控,NW 向先存断裂活化,分割凹陷;强烈断陷阶段,NNE—NE 向强伸展与弱走滑叠合,NNE 向强伸展-弱走滑断裂变为主控,NW 向断裂活动减弱或停止;走滑坳陷阶段,NNE 向强走滑与弱伸展叠合,断裂不控制沉积,但对地层展布具有调整作用。③研究区伸展-走滑叠合断裂的发育演化与油气成藏密切相关,整体具有“早期伸展控源、晚期走滑控运、多期叠加控圈”的特征,东部斜坡带是油气运聚的有利区。
中图分类号:
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