The calculation of such a 1D model in…

The calculation of such a 1D model in conjunction with the checking and selection of the earthquake data is a tedious procedure. However, the calculation an testing of the minimum 1D model is an integral part of the 3D inversion, since the linearization of the inverse problem is based in part on the assumption of well-located events.

Geotomography with local earthquake data, Kissling, 1988