摘要
本文在总结断裂带构造格局的基础上对断裂几何学及运动学进行深入分析,并通过断层生长指数、古落差的研究,证明了汉留断层的走滑性质及其既有持续生长的特点又有幕式活动的特点。理顺了该区的断层级别序次和组合样式并在此基础上提出了该区构造模式,即汉留断层和真武分支断层的几何形态以及两者的搭配关系产生的不同应力场,分为四个区域,每个区域具有不同的断层组合形式。
Based on analysis of fault geometry and kinematics,and combined with growth index and paleo fall of fault,it is demonstrated that strike-slip of Hanliu fault has not only characteristics of sustained growth but also characteristics of episodic migration.On the basis of the district-level fault sequence and style of combination,it was proposed to a structural model for this region,that is different stress fields created by collocation and geometric configuration of Hanliu fault and Zhenwu branch fault,which can be divided into four regions with different combinations of fault.
出处
《复杂油气藏》
2010年第2期5-7,共3页
Complex Hydrocarbon Reservoirs
基金
江苏石油勘探局(JS07010)
关键词
汉留断层
走滑断层
断层生长指数
断层古落差
构造模式
HanLiu fault
strike-slip of fault
growth index of fault
paleo-fall of fault
tectonic model