利用断层围陷波资料研究龙门山断裂带分段特征
Recent Developments in World Seismology（2018）
Abstract
断层围陷波(Fault zone trapped waves)又称为断层通道波、断层导波、槽波,是波在断层的两个边界内侧多次反射并相干迭加而形成的.围陷波既然是由断层带内低速介质和高速围岩之间的相干多次反射波构成的,那么其振幅和频率就强烈地依赖于断层带内介质的物理性质和断层的几何形态.所以观测、分析和模拟断层围陷波能够确定断层的深部细节.
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