石油与天然气地质 ›› 2022, Vol. 43 ›› Issue (6): 1347-1358.doi: 10.11743/ogg20220606
• 油气地质 • 上一篇
收稿日期:
2022-03-21
修回日期:
2022-09-08
出版日期:
2022-12-01
发布日期:
2022-11-21
第一作者简介:
王冰洁(1984—),男,博士、工程师,石油地质和勘探。 E-mail:基金项目:
Bingjie Wang(), Deying Wang, Xin Wang, Guanzhou Hui, Mingwang Xue
Received:
2022-03-21
Revised:
2022-09-08
Online:
2022-12-01
Published:
2022-11-21
摘要:
渤海湾盆地辽中凹陷南洼发育走滑转换带,是大、中型油田形成的有利位置。利用三维地震资料解释结果,结合勘探实践,对该区走滑转换带的特征及构造圈闭的形成、古近系砂体展布和油气垂向运移这3个成藏要素进行分析。结果表明:①依附于5条走滑断层,研究区形成了断边走滑转换带、断间走滑转换带和断梢走滑转换带3种类型,每种又可分为压扭型和张扭型2个亚类,对应形成增压型和释压型构造圈闭;②压扭型走滑转换带发育的构造圈闭规模大(即增压型的构造圈闭面积大),为大、中型油田的形成提供了有利的圈闭条件;③走滑转换带古近系砂体在走滑作用下表现出明显的迁移性,导致其在横向上分布范围更广,可接受来自不同位置烃源岩的原油充注,在平面上形成多构造含油的特征;④走滑转换带伴生调节断层发育,有利于油气的垂向运移,最终形成多层系和多断块含油的特点。综上所述,辽中凹陷南洼走滑转换带控制了大规模构造圈闭的形成、控制了古近系砂体在横向上的分布以及原油在垂向上的运移等大、中型油田形成的基本成藏要素。
中图分类号:
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