论文部分内容阅读
利用位于金州断裂两侧地震台所记录的地震震级的差异，研究金州断裂的降震效应。统计表明，当地震波通过断裂时存在明显的衰减现象，震级相差近０．４级。
Using the difference in the magnitude of earthquakes recorded by seismographs located on both sides of the Jinzhou fault, the quake-reducing effect of the Jinzhou fault is studied. Statistics show that there is a clear attenuation phenomenon when the local seismic waves pass through the fault, and the magnitudes of the earthquakes are almost 0.4.