石油与天然气地质 ›› 2021, Vol. 42 ›› Issue (5): 1056-1062.doi: 10.11743/ogg20210504
收稿日期:
2021-03-05
出版日期:
2021-10-28
发布日期:
2021-10-26
作者简介:
何发岐(1967-), 男, 博士、教授级高级工程师, 石油天然气勘探开发及管理。E-mail: 基金资助:
Faqi He(), Rong Qi, Fubin Wang, Jie Deng, Li Cheng, Tianle Hu
Received:
2021-03-05
Online:
2021-10-28
Published:
2021-10-26
摘要:
鄂尔多斯盆地南部镇泾地区延长组顶部广泛发育沟谷体系,前人多认为是风化剥蚀和河流侵蚀所致。为了进一步厘清沟谷体系的发育特征、分布规律及其与区域构造的联系,基于三维地震资料对断裂的解释和前侏罗纪古地貌的恢复,刻画了延长组沟谷体系,探讨了其构造成因。结论显示,在延长组沉积晚期,受SW向区域构造挤压作用,玉都断裂发生左旋走滑,使延长组未成岩地层发生塑性变形,形成了一系列NW-SE向展布的挤压隆起与谷地;同时NW-SE向的拉张作用形成了NE-SW向的伸展谷地,最终形成了延长组晚期广泛分布的沟谷体系格局。该认识对于鄂尔多斯盆地南部延长组及其上覆的延安组的油气勘探都具有一定的指导意义。
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