地震台站面波震级台基校正值测定  

Measurement of correction value of station basement for surface wave magnitude of seismic station

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作  者:包淑娴[1] 刘瑞丰[1] 孙丽[2] 王丽艳[1] 杨辉[1] 邹立晔[2] Bao Shuxian;Liu Ruifeng;Sun Li;Wang Liyan;Yang Hui;Zou Liye(Institute of Geophysics, China Earthquake Administration, Beijing 100081, China;China Earthquake Networks Center, Beijing 100045, China)

机构地区:[1]中国地震局地球物理研究所,中国北京100081 [2]中国地震台网中心,中国北京100045

出  处:《地震地磁观测与研究》2016年第4期49-56,共8页Seismological and Geomagnetic Observation and Research

基  金:地震行业专项(项目编号:20070824;20070837)

摘  要:利用中国地震台网1985—2001年面波资料,基于该台网使用的面波震级计算公式,计算64个地震台站面波震级台基校正值,结果表明:地震台站受所在地区地壳结构、近地表岩石性质、土壤疏松程度、地形等因素影响,大部分台站校正值在±0.2之内,最大校正值为-0.31。On the basis of the formula of surface wave magnitude and the data of surface wave recorded by Chinese seismograph network during 1985 to 2001, the correction values of station basement for surface wave magnitude of 64 stations were calculated. The results showed that, as the influence of crustal structure, properties of rocks near surface, soil porosity, topography and other factors of seismologic stations in different regions, the correction values in most of seismic stations are smaller than ± 0.2, and the maximum is -0.31.

关 键 词:地震台站 量规函数 面波震级 台基校正 

分 类 号:P315.32[天文地球—地震学]

 

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