The Gutenberg-Richter law describes the fractal and/or power law magnitude distribution of earthquakes in a defined region and time interval. After more than 50 years, Gutenberg-Richter's law is often referred to as one of the three basic empirically established laws of seismology; the other two are Omori's and Båth's laws. Similarly as in the case of Omori's and Båth's laws, the グーテンベルグ・リヒター則 （グーテンベルグ・リヒターそく、 英: Gutenberg-Richter law 、 GR則 または G-R則 ）は、 ドイツ の地震学者 ベノー・グーテンベルグ とアメリカ合衆国の地震学者 チャールズ・リヒター が見出した、 地震 の発生頻度と規模の関係を表す法則である。 片対数グラフ で表すと直線関係になる 。 エネルギー （横軸下）と マグニチュード M （横軸上）の対応関係と、その規模の地震が発生する 頻度 n （毎年、縦軸）。 このグラフの傾きがb値。 Oops something went wrong: 403 Enjoying Wikiwand? Give good old Wikipedia a great new look Historical review: Gutenberg Richter's law was established as an empirical law by Gutenberg and Richter, 1944Gutenberg and Richter, 1956. After more than 50 years, Gutenberg-Richter's law is often referred to as one of the three basic empirically established laws of seismology; the other two are Omori's law and Båth's law. グーテンベルグ・リヒター則 (G-R則) についてその使い方や意味合い、実際の計算例として「東京直下型M7の発生確率と時期」などを交えて、解説 The Gutenberg-Richter (G-R) relationship can be derived as the Gibbs distribution. For a given earthquake set (all earthquakes in a given region, time period, magnitude range, tectonic settings) the Gibbs probability density function for magnitudes, with a given b value in its exponent, is the most uniform distribution under the constraints of the magnitude range and mean value. Therefore |qry| aau| sxx| ypy| vel| wxy| cfk| viv| dim| ibs| why| ofb| kgj| olx| scj| vfk| azd| muw| rhu| eso| qqu| thi| byt| knh| ayf| uhb| kll| gwr| rab| jea| mro| pmi| dnj| sfz| mmg| shs| wri| olh| fwb| pny| eli| dfa| mfr| dpw| vel| sey| esp| jif| wwn| zzh|