【摘要】 根据历史地震资料的考证结果,734年天水地震的极震区位于秦州中都督府、麦积都尉一带,今天水市秦城区、北道区和麦积山一带,震中烈度达Ⅹ度,震级71/2级左右。其等震线长轴方向为NW向,大致与西秦岭北缘断裂带的甘谷-武山断裂段相吻合,极震区正好位于甘谷-武山断裂段的东端。综合分析认为,734年天水71/2级地震的发震构造为西秦岭北缘断裂带的甘谷-武山断裂段东端。更多还原

【Abstract】 Tianshui area locates at the northeastern margin of Qinghai-Tibetan plateau and the middle segment of the north margin of western Qinling tectonic zone.In history,several strong destructive earthquakes happened in the area.Because of the very long history and that the historical records are not quite clear,it is very difficult to study them in nowadays,and most of them became historical knotty problems.The Tianshui earthquake in 734 AD is one of the large earthquakes.On March 23,734 AD,a large earthquake happened in Qinzhou of Tang Dynasty,now the vicinity of Tianshui City,causing serious seismic disasters as “the earth ruptured and closed again,nearly all the houses damaged,about 4000 people dead,hills changed into valleys,and towns covered by landslip,and so on”.According to the detail textual research of the historical earthquake records,the meizoseismal area of the 734 AD Tianshui earthquake is in the Qinzhou and Maiji area,now,the Qincheng,Beidao and Maijishan area of Tianshui City.The epicenter intensity is about Ⅹ,the magnitude is about M 71/2.The direction of long axis of isoseismal line is NW,consistent with the strike of the eastern segment of Wushan-Gangu Fault of the northern margin of western Qinling active fault zone.The meizoseismal area is just in the step-over zone between the left-lateral strike-slip faults,i.e.the Tianshui-Baoji Fault and the Gangu-Wushan Fault,an area prone to strong earthquake.Comprehensive analysis indicates that the causative structure of the 734 M71/2 Tianshui earthquake is the east segment of the Gangu-Wushan Fault of the northern margin of western Qinling active fault zone.更多还原