地震地质 ›› 1987, Vol. 9 ›› Issue (2): 17-25.

• 论文 • 上一篇    下一篇

震源断裂规模与震级的定量关系

叶文华   

  1. 国家地震局地质研究所
  • 收稿日期:1985-07-31 出版日期:1987-06-02 发布日期:2009-11-25

QUANTITATIVE REALTIONSHIP BETWEEN THE SOURCE PARAMETERS AND THE EARTHQUAKE MAGNITUDES

Ye Wen-hua   

  1. Institute of Geology, State Seismological Buieau
  • Received:1985-07-31 Online:1987-06-02 Published:2009-11-25

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MLMs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