Abstract The clearest statistical signal in aftershock locations is that most aftershocks occur close to their mainshocks. More precisely, are triggered at distances following a power-law decay distance (Felzer and Brodsky, 2006). This kernel used epidemic-type sequence (ETAS) modeling typically assumed be isotropic, even though individual sequences show more clustered occurrence. assumption of...

Analyzing the tables and probability maps posted by Yan Y. Kagan and David D. Jackson in April 2002–September 2004 at http://scec.ess.ucla.edu/~ykagan/predictions_index.html and the catalog of earthquakes for the same period, the conclusion is drawn that the underlying method could be used for prediction of aftershocks, while it does not outscore random guessing when main shocks are considered....

Abstract The 2019 Mw 7.0 Banten, Indonesia, earthquake occurred at a 49 km depth in relatively unknown region, where the geological structure did not clearly show fault. In this study, we use Global Navigation Satellite System data to analyse fault source of earthquake. Following earthquake’s focal mechanism, modelled total four models using two possible strikes, with each strikes investigated ...