作者:Konstantina A. Papadopoulou,Efthimios S. Skordas,Nicholas V. Sarlis
摘要:Using the order parameter of seismicity defined in natural time, we suggest a simple model for the explanation of B?th law, according to which a mainshock differs in magnitude from its largest aftershock by approximately 1.2 regardless of the mainshock magnitude. In addition, the validity of B?th law is studied in the Global Centroid Moment Tensor catalogue by using two different aftershock definitions. It is found that the mean of this difference, when considering all the pairs mainshock-largest aftershock, does not markedly differ from 1.2 and the corresponding distributions do not depend on the mainshock's magnitude threshold in a statistically significant manner. Finally, the analysis of the cumulative distribution functions provides evidence in favour of the proposed model.
發文機構:Section of Solid State Physics Solid Earth Physics Institute
關鍵詞:解釋模型地震活動定律時間自然序參量累積分布函數震級Bath law . Aftershocks .Order parameter .Natural time
分類號: P631.84[天文地球—地質礦產勘探][天文地球—地質學]P315.5[天文地球—地震學][天文地球—固體地球物理學][天文地球—地球物理學]