• 责任者：Wu Mingda (Earthquake Administration of Liaoning Province ; Shenyang 110034 ; China) ; Zhong Yizhang
• 刊名：Earthquake Research in China
• 出版年：2009
• 卷期：25(2)
• 关键词：深部构造 ; deep-seated structure ; 地震活动性 ; seismicity ; 表壳构造 ; superstructure ; 辽宁 ; Liaoning Province
• 页码：p.132-139
• 图表：3 illus., 2 refs.
• 分类号：0500
• issnNo：ISSN1001-4683
• isbnNo：CN11-2008/P

The deep and shallow tectonic data in Shenyang and the relationship with the seismic activities show that the developed northeast faults have controlled the formation and the development of the fault-uplift and fault-concave. The uplift and concave of the bedrock below 7 km underground were consistent with the surface structure and two deep faults developed in the lower crust. Because of the deep incision and new activities, the surface Wanggangbao-Xinchengzi fault and Yongle-Qingshuitai fault, which correspond to the deep F₃ fault and F₆ fault, might be related with seismic activities in Shenyang.