地震地磁观测与研究Issue(3)：38-42,5.DOI:10.3969/j.issn.1003-3246.2015.03.007
青海地区S波非弹性衰减Q值、场地响应特征研究
S wave inelastic attenuation and site response in Qinghai area
摘要
Abstract
According to the geological structure the distribution of observation network,Qinghai area was divided into three subregions,including Qaidam Basin,the northeastern and southeastern of Qinghai. Based on the 112 digital seismic waveforms data recorded by Qinghai network,the inelastic attenuation Q value with frequency of these subregions are inversed by Atkinson’s genetic algorithm,showing that the Q value of Qaidam Basin is maximum while the southeastern is minimum. Site responses of 24 stations in these subregions are inversed using the Moya method, the results indicate that site responses of 15 stations are uneven in frequency domain,the others have better stability,and as a standard station,GOM station has better observation conditions, making the site responses has no magnification nearly in frequency domain.关键词
Q值/场地响应/几何衰减Key words
Q value/site response/geometrical attenuation引用本文复制引用
马建新,姚家骏,陈继锋..青海地区S波非弹性衰减Q值、场地响应特征研究[J].地震地磁观测与研究,2015,(3):38-42,5.基金项目
地震科技星火计划（XH14050Y）、青海省地震科学基金（2012A04）联合资助 （）
