口泉断裂带中段断裂组合特征及活动性研究
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摘要
为查明口泉断裂在圣水沟—鹅毛口段断裂特征和断裂活动性,野外采用了地质调查、人工地震勘探、电阻率CT法、钻孔控制等综合手段对该段内的断裂具体位置、断裂活动性进行了详细研究,从而避免断裂活动对建筑物产生破坏。
In order to check the fracture features of Kouquan faults in the Shengshuigou to Emaokou and fracture activity,the paper uses the comprehensive measures in the open air,including geological survey,the artificial seismic exploration,the resistance tomography method,the borehole control,to undertake a detailed study on the actual position and the fracture activity of the fraucture in this segment,in order to avoid its damage to the buildings.
引文
[1]谢新生.山西大同盆地口泉断裂全新世古地震活动[J].地震地质,2001,25(3):11-12.
    [2]王阁,张季超,吴冬梅.城市地质环境灾害的信息化分析[J].山西建筑,2007,33(8):126-127.

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