New Ability for Analysis of the Focus Zone of the Crust Seismic Events
The initial goal of this work was to improve the location algorithms used to determine the depth of crustal events. Eventually, it became apparent that we were incapable of determining the depth of what is required. The location problem has solutions based on Geiger methods. Iteration procedures are used to solve this mathematical task that is purely mathematical. The mean square residual is the criteria used to conclude the iteration procedure. The physical problem of estimating the origin location and impact of the following earthquake on surrounding environments has not been addressed by any of them. It’s clear that the impact is dependent on radiation during seismic activity. From the other side, the beginning of the seismic events is determined by the set of arrival times, which is the sole instrumental evidence of the process. So it is clear that having kinematic parameters, such as arrival times, is necessary to determine a dynamic solution. Sure, the seismic records are available for use. At this time, it has been recognized that a new algorithm is required to identify the location with the most seismic energy radiation. The first arrival times must be matched to this location. Secondly, the internal structure of a focus zone must be decomposed by seismic energy using the new algorithm. During the investigation it appears that travel time tables have self-organized structures.
