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福建顺昌尾波Q值衰减特征初探
引用本文:陈光,陈金鹏. 福建顺昌尾波Q值衰减特征初探[J]. 高原地震, 2009, 21(2): 24-27
作者姓名:陈光  陈金鹏
作者单位:福建省地震局,福建,福州,350003;广东省水利水电第三工程局,广东,东莞,523710
摘    要:基于Sato单次散射模型,利用2007年3月13日福建数字地震台网记录的发生在福建省北部地区的45条ML≥2.0级地震波形资料,对福建北部地区尾波Q值进行了研究,研究中首先计算各条记录尾波4—18Hz间15个频率的尾波Q值,并对Q值与频率之间的依赖关系进行拟和,拟和结果为:Qc(f)=(150.34±42.51)f^(0.8214±0.2109)。

关 键 词:尾波Q值  Sato模型  福建北部

CHARACTERISTICS OF CODA WAVE ATTENUATION IN SHUNCHANG AREA IN FUJIAN PROVINCE
CHEN Guang,CHEN Jinpeng. CHARACTERISTICS OF CODA WAVE ATTENUATION IN SHUNCHANG AREA IN FUJIAN PROVINCE[J]. Plateau Earthquake Research, 2009, 21(2): 24-27
Authors:CHEN Guang  CHEN Jinpeng
Affiliation:1. Earthquake Administration of Fujian Province, Fuzhou 350003, China ; 2. The No. 3 Water Conservancy and Hydro - Electric Engineering Bureau of Guangdong Province, Dongguan 523710, China)
Abstract:Based on the single scatter mode ( Sato), using 45 earthquake digital wave data of ML≥ 2. 0 earthquakes in north area of Fujian province since Mar. 13,2007 recorded by Fujian earthquake digital network, the average Q value of coda in relative region is calculated, and the relationship between Q value and frequency is fitted. The result is that Qc(f)=(150.34±42.51)f^(0.8214±0.2109).
Keywords:Q value of coda  Sato model  North area of Fujian province
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