石油学报 ›› 2022, Vol. 43 ›› Issue (11): 1542-1557.DOI: 10.7623/syxb202211003
管树巍1, 姜华1, 鲁雪松1, 梁瀚2, 朱光有1, 崔俊峰1, 金惠1, 雷明1, 陈涛4, 杨荣军4
收稿日期:
2022-03-15
修回日期:
2022-08-08
出版日期:
2022-11-25
发布日期:
2022-12-02
通讯作者:
管树巍
作者简介:
管树巍,男,1970年6月生,2004年获浙江大学博士学位,现为中国石油勘探开发研究院高级工程师,主要从事含油气盆地构造分析工作。Email:guan@petrochina.com.cn
基金资助:
Guan Shuwei1, Jiang Hua1, Lu Xuesong1, Liang Han2, Zhu Guangyou1, Cui Junfeng1, Jin Hui1, Lei Ming1, Chen Tao4, Yang Rongjun4
Received:
2022-03-15
Revised:
2022-08-08
Online:
2022-11-25
Published:
2022-12-02
摘要: 四川盆地中部(川中地区)的走滑断裂与多层系油气聚集关系密切。系统阐述走滑断裂的性质、特征、分布规律、成因与演化机制对于深化川中地区断裂系统控藏与控富集研究,以及完善四川盆地复合含油气系统理论具有重要意义。研究在川中地区下—中三叠统膏盐岩层内部识别出深层走滑断裂的伴生构造,以及导致上震旦统灯影组台缘错动的走滑断裂行迹。研究表明,深层走滑断裂与其伴生构造之间存在2种组合关系,据此识别出6条主干左行走滑断裂带。通过分析代表性生长构造的局部构造活动(LSA)沉降量变化,将川中地区的断裂演化划分为5个阶段:1晚震旦世同沉积断裂阶段;2早奥陶世—早二叠世右行走滑阶段;3晚二叠世—早三叠世伸展走滑断裂阶段;4中—晚三叠世走滑活动沉寂阶段;5中侏罗世至今左行走滑阶段。走滑断裂是控制川中地区多层系立体差异化成藏的关键因素。在晚二叠世—早三叠世伸展走滑断裂阶段,安岳裂陷槽内筇竹寺组烃源岩进入生油高峰,原油沿灯影组台缘及NWW向断裂带充注成藏;在中侏罗世至今左行走滑阶段,特别是晚白垩世以来,深层走滑活动在下—中三叠统膏盐岩层及上覆地层内形成伴生构造,控制了浅层陆相致密油气的分布,同时派生出的NE向伸展破裂则造成深层原油裂解气垂向运移至龙王庙组,甚至在栖霞组、茅口组聚集成藏,形成"上富下贫"的油气成藏模式。
中图分类号:
管树巍, 姜华, 鲁雪松, 梁瀚, 朱光有, 崔俊峰, 金惠, 雷明, 陈涛, 杨荣军. 四川盆地中部走滑断裂系统及其控油气作用[J]. 石油学报, 2022, 43(11): 1542-1557.
Guan Shuwei, Jiang Hua, Lu Xuesong, Liang Han, Zhu Guangyou, Cui Junfeng, Jin Hui, Lei Ming, Chen Tao, Yang Rongjun. Strike-slip fault system and its control on oil & gas accumulation in central Sichuan Basin[J]. Acta Petrolei Sinica, 2022, 43(11): 1542-1557.
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