邯郸—邢台地区尾波衰减特征研究  

Study on the characteristics of coda wave attenuation in Handan-Xingtai area

作　　者：张小涛[1] 马广庆[1] 孙晴[1] 韩丽萍[1] 吕凤章[1] 宋增良[1] 

机构地区：[1]河北省地震局邯郸地震中心台

出　　处：《华北地震科学》2007年第2期29-32,共4页North China Earthquake Sciences

摘　　要：中文摘要 利用红山数字地震台和邯郸数字台网记录到的2001年3月-2006年7月近震波形资料,采用Aki的尾波单次散射模型计算了邯郸—邢台地区不同尾波窗长的Qc值,窗长为20s时该区域的平均值为Qc=78f^0.92,40s时Qc=144f^0.88。在研究范围内呈现出北高南低的态势。Based on Aki single scattering model, the Qc values with different coda window in Handan-Xingtai area are calculated with the seismic wave data recorded by Hongshan Seismostation and Handan digital Seismic network from March of 2001 to July of 2006. The mean Qc value is 78f^0.92 ,when window length is 20s,and is 144f^0.88 ,when window length is 40s. The Qc value is high in south and low in north.

关 键 词：散射模型 尾波 QC值 介质 

分 类 号：P315.3[天文地球—地震学]