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济阳坳陷东部走滑构造形成机制
引用本文:胡贤根 谭明友 张明振. 济阳坳陷东部走滑构造形成机制[J]. 油气地球物理, 2007, 5(1): 50-54,58
作者姓名:胡贤根 谭明友 张明振
作者单位:胜利油田分公司物探研究院,257022
摘    要:地震资料表明济阳坳陷东部存在走滑断层。依据切割深度将其分为深层次和浅层次两种,并分别论述了它们的特点和分布规律。引入脆性层次走滑断层单剪模式,从理论上分析了该区走滑断层形成的应力机制及演化过程。

关 键 词:走滑构造  郯庐断裂  济阳坳陷东部
修稿时间:2006-08-262006-11-11

The strike-slip structure in the east of Jiyang Depression
Hu Xian-gen. The strike-slip structure in the east of Jiyang Depression[J]. Petroleum Geophysics, 2007, 5(1): 50-54,58
Authors:Hu Xian-gen
Affiliation:Geophysical Research Institute of Shengli Oilfield Branch Co.,Dongying 257022, China
Abstract:The seismic data shows the existence of strike-slip structure in the east of Jiyang Depression, divided into deep and shallow formation faults by cut depth. The characteristic and distribution of two kinds of faults are discussed. Importing the single-shear mode of brittle strike-slip fault, the stress mechanism and evolvement of strike-slip faults in this area are analyzed theoretically.
Keywords:strike-slip structure   Tanlu faulted zone and theeast of Jiyang Depression
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