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Comparison between earthquake magnitudes determined by China seismograph network and US seismograph network (II): Surface wave magnitude

机译:中国地震仪网和美国地震仪网确定的地震震级比较(二):表面波震级

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摘要

By using orthogonal regression method, a systematic comparison is made between surface wave magnitudes determined by Institute of Geophysics of China Earthquake Administration (IGCEA) and National Earthquake Information Center of US Geological Survey (USGS/NEIC) on the basis of observation data collected by the two institutions between 1983 and 2004. A formula is obtained which reveals the relationship between surface wave magnitudes determined by China seismograph network and US seismograph network. The result shows that, as different calculation formulae and observational instruments are used, surface wave magnitude determined by IGCEA is generally greater by 0.2 than that determined by NEIC: for M=3.5∼4.5 earthquakes, it is greater by 0.3; for M=5.0∼6.5 earthquakes, it is greater by 0.2; and for M≥7.0 earthquakes, it is greater by no more than 0.1.
机译:利用正交回归方法,根据中国地震局地球物理研究所(IGCEA)和美国地质调查局国家地震信息中心(USGS / NEIC)确定的表面波幅值,进行了系统比较。在1983年至2004年这两个机构之间,获得了一个公式,揭示了中国地震仪网络和美国地震仪网络确定的表面波幅值之间的关系。结果表明,由于使用了不同的计算公式和观测仪器,由IGCEA确定的地表波幅通常比由NEIC确定的地表波幅大0.2:对于M = 3.5〜4.5级地震,地表波幅值大0.3。对于M = 5.0〜6.5地震,它要大0.2。对于M≥7.0的地震,其不超过0.1。

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