• 责任者：Yan Chengguo (Tianjin Earthquake Administration ; Tianjin 300201 ; China) ; Chen Yukun
• 刊名：Seismology and Geology
• 出版年：2013
• 卷期：35(4)
• 关键词：断裂 ; fractures ; 隐伏构造 ; subsurface structure ; 声波法 ; acoustical methods ; 天津 ; Tianjin
• 页码：p.745-753
• 图表：6 illus., 7 refs.
• 分类号：0300
• issnNo：ISSN0253-4967
• isbnNo：CN11-2192/P

     Qikou depression is an important tectonic unit in the eastern part of the Huanghua depression,which constitutes the Cenozoic depocenter,with the Cenozoic maximum deposition thickness reaching to 8000 ～ 10,000m.Several profiles of acoustic survey have been conducted across the buried faults in Tianjin Qikou depression.The surveying results show that the high-angle near EW trending normal faults are well developed.The latest upper break points of these faults are 35m from the seabed,being very shallow,and the dislocated stratums are very new.Combined with regional stratigraphic analysis,the buried faults should be late Pleistocene active faults.But the deep seismic profiles reveal that these faults in shallow strata appear as negative flower structures,which form a compound graben structure,and gradually integrate into the Qibei Fault and Haihe Fault in the deep part,as branch faults of Qibei Fault and Haihe Fault.So,these faults don＇t have great tectonic significance,as the normal faults associated with the coseismic slip at the shallow strata when earthquakes occurred at the deep part of Haihe Fault.The earthquake risk assessment of these faults should be different from other active faults.We can＇t think they have a high seismic risk,just because they are late Pleistocene active faults.But,there is a high seismic risk for the Haihe Fault.The deep seismic profiles show that Haihe Fault and Haiyi Fault are boundary faults of Qikou depression,Qibei Fault and Qizhong Fault are the secondary faults within Qikou depression; Haihe Fault is shown as a listric normal fault on the seismic profile,and in its shallow part,multiple shallow branch faults are developed,which control the Cenozoic sedimentary development of Qikou depression.The Qibei Fault is the main branch of Haihe Fault,and as shown on the acoustic shallow stratigraphic profiles,it is a late Pleistocene active fault,though it is smaller in size relative to Haihe Fault,we can＇t ignore the seismic risk of Qibei Fault.