Matrix method in the problems of calculation of the earthquake wave-field and parameters of its source
The construction of a field displacement on the free surface of layered medium using the matrix method of Thomson – Haskell is considered. The authors show the obtained solution of the direct problem of seismology. The analytical solutions of the direct problem are used for solving the inverse problem. This method of solving of the inverse problem allows the source distributed in time and definition of the time function of the source STF to be considered.