地震地质 ›› 1987, Vol. 9 ›› Issue (2): 17-25.
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叶文华
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Ye Wen-hua
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摘要: 研究震源参数(震源断裂规模)与震级的定量关系必须考虑震级的物理含义。本文利用我国海城地震、唐山地震前后的151个小震(1.5≤ML≤3.9)和国内外58个浅源的中、强震(4.4≤Ms≤8.2)资料,得到了一组稳定的、互相一致的震源断裂参数与震级ML和Ms的函数关系。由此讨论了常用震级ML、Ms与mb之间的关系。新的震源参数与震级关系表明,震源断裂规模如断裂长度、面积或错距等与面波震级Ms和近震震级ML不存在一一对应的比例关系。
关键词: 震源参数, 近震震级, 面波震级
Abstract: The physical significance of earthquake magnitudes must be considered when studing the quantitative relationship between the source parameters and earthquake magnitudes. In this paper, a set of stable, uniform functional relations of the source fracture parameters to magnitudes ML and Ms have been obtained by using the data of 151 smaller earthquakes (1.5≤ML≤3.9) preceding and following Hai Cheng and Tangshan earthquakes as well as 58 moderate and strong shallow earthquakes(4.4≤Ms≤8.2) on the earth. The relation between the magnitudes ML, Ms and mb is discussed as well.The alternative relationship between the source fracture parametes and earthquake magnitudes shows no proportional one-to-one correspondence between the source fracture size of earthquake (i. e fault length, fault area or dislocation etc.) and surface wave magnitude Ms and local magnitude ML.
Key words: Source parameter, Local magnitude, Surface wave magnitude
叶文华. 震源断裂规模与震级的定量关系[J]. 地震地质, 1987, 9(2): 17-25.
Ye Wen-hua. QUANTITATIVE REALTIONSHIP BETWEEN THE SOURCE PARAMETERS AND THE EARTHQUAKE MAGNITUDES[J]. SEISMOLOGY AND GEOLOGY, 1987, 9(2): 17-25.
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https://www.dzdz.ac.cn/CN/Y1987/V9/I2/17