Once stress is altered, the rock properties change, and sensing, time after time, selects target zones
in rocks by the changed elastic characteristics in them, while the other, larger part of the seam, which is
stable and uninteresting in terms of the formulated task, remains beyond the scope. We consider this
the first time formulated in the mine seismics approach an integration of the seismic tomography and
the force impact on rocks into one package.