Part of #SCALING OF LONG-TERM SEISMICITY IN ZAGROS, IRAN# :
Publishing year : 2011
Conference : 6th International Conference on Seismology and Earthquake Engineering
Number of pages : 8
Abstract: The phenomenon involves an increase in the magnitude and frequency of minor earthquakes in an area near the location of a major event by the long-term precursor scale increase phenomenon. The modeling of long-term seismogenesis as a three-stage faulting process against a background of self-organized criticality can be deduced from a predictor scale increase.