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《Earthquake》 2002-03
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The crustal vertical deformation and the action of future strong earthquake in Capital Circle Area

YANG Guo hua, HAN Yue ping,XIE Jue min,ZHOU Xiao yan (The First Crustal Deformation Monitoring Center,Tianjin 300180,China)  
Crustal vertical deformation and its characteristics in the past decade have been analyzed according to precise re leveling data in the capital circle area.The result indicates that large special and magnitude ground subsidence happened in Beijing,Tianjin,Hebei plain and other regions because of over pumping groundwater,so the tectonic movement information in these areas can't be got and the crustal motion information can be got only in northeastern region and western region of the capital circle area.The northeastern part,i.e.the east and north of Tangshan Zunhua Xinglong,shows subsidence with 2 4mm/a,but the movement situation with rise in the northern part and subsidence in the southern part has not been always changed.The part of western region shows uplift with 10mm/a,the western part is referred to Taihang Mountain.The movement situation has changed from uplifting for the whole region with fast speed in the south and that with slow speed in the north to some uplifting in the north and some subsiding in the south.2001 year is the dividing line that the movement in west region changed.Obvious four quadrant deformation happened in Yanhuai basin and its adjacent areas.Although its scale and magnitude are smaller than that of Datong region before Datong earthquake,their movement patterns are very similar.It could be inferred that strong earthquake might occur in this part in the future.
【Fund】: 国家重点基础研究发展规划项目 (G1 9980 40 70 3 )
【CateGory Index】: P315.72
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