山西临猗-永济1998年5.0级地震宏观烈度考察报告
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摘要
叙述了对山西省临猗—永济1998年7月11日发生的ML50地震宏观烈度的调查情况,得出这次地震的极震区烈度为Ⅵ度,呈椭圆形,长轴走向NNW,长度21km,短轴17km,面积280km2的结论。阐述了地震发生区域的构造环境,分析了发震构造,认为震区NEE向的临猗—双泉断裂、中条山北麓断裂为控制运城盆地的边界断裂,属区域主干活动断裂;NNW向孙常断裂为盆地内的隐伏断裂,属次级活动断裂,推测该断裂为临猗—永济地震的发震断裂。
The situation of the macroseismic intensity survey for the M L5 0 Linyi-Yongji earthaquake was recounted,the conclusion was obtained that the intensity of the meizoseismal region is Ⅵ degree,a ellipse,the strike of its long axis is NNW,the length 21 km,the short axis 17 km,the area 280 km 2.The tectonic condition of the seismogenic zone was recounted,the statutory was analyzed.It was suggested that Linyi-Shuangquan fracture and the fracture of the north piedmont in Zhongtiao mountain are the boundary fractures controlled Yuncheng basin,belong to the main active fracture in the region,Sunchang fracture of NNW strike is the buried fracture in the basin,belongs the second-order active fracture,the fracture is inferred the seismogenic fault of the Linyi-Yongji earthquake.
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