断层围陷波
断层围陷波
经过数字滤波和频谱分析等技术, 由地震记录图中分离出了断层围陷波。
Based on the fault zone trapped waves observed in Kunlun Mountain Pass region, the width of the rupture plane is deduced to be about 300 m and is greater than that on the surface.根据昆仑山口西地震测线断层围陷波的观测结果,可推断该处破裂面宽度为300 m左右,远远大于地表破裂带的宽度。