Method of Some Inverse Geophysical Problem Solution by Using Weakly Coupled Connected Distributed Computing Systems

In this work a possible model for organizing a grid-based application that performs the solution of several inverse geophysical problems is described. As an example, we consider the problem of determining the parameters of seismic anisotropy in the Earth's mantle by the inversion of seismic waveforms. It is shown that this class of problems is reduced to the tabulation of a complicated multidimensional function. In this approach, the calculation at each point in a definition interval is calculated independently, so this is ideally appropriate for calculations that use a loosely connected distributed computing infrastructure.