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《Hydrogeology and Engineering Geology》 2003-05
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Tectonic subsidence and prospect of ground subsidence control in Tianjin area

WANG Ruobai\+1,ZHOU Wei\+1,LI Feng\|lin\+2,WANG Hong\+2,YANG Gui\|ye\+3,YAO Zhong\|jie\+3,KUANG Shao\|jun\+3(1.The First Crustal Deformation Monitoring Center, CSB, Tianjin300180, China; 2.Institute of Geology and Mineral Resources of Tianjin, Tianjin300170, China; 3.Working Office of Ground Subsidence Control of Tianjin, Tianjin300042, China)  
By the means of Quaternary geology, statistical geomorphology and historical bench mark investigation, the background of tectonic subsidence and the prospects of the subsidence control in Tianjin area are studied. Based on a series of data related to the depth of the first marine layer bottom, the borehole of Holocene, the deep lift marks of bedrock and the historical bench marks in Tianjin area, the average velocity of tectonic subsidence is 1.7mm/a has been obtained. Moreover, some laws for the background of basement tectonics subsidence have been discovered from the research as follows: (1) The tectonic subsidence has a trend of gradual increase from the western region to the eastern coast. (2) An anomalous tectonic subsidence zone in the northwest direction is developed along the Haihe River. (3) It is proved by all kinds of data that the directions of subsidence are different with boundary of the Haihe River. The contour lines extend mainly in NWW in the northern part and NE in the southern part. The law of entire activity has reflected the controlling effect by the active faults and base structure. 
【Fund】: 天津市建委资助项目(98-025)
【CateGory Index】: P642.26
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