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Deforming processes in areas of geologic failures (tectonic faults, boundary zones of block structures etc.) have the singularities in comparison with those, flowing past on "quiet" sites of rock masses. The intensive assimilation of underground space in most cases reduces in a modification of structural organization of a mining massif. In turn development of new structures or "revival" old is accompanied by adjustments on growing or available faults and is exhibited as strains of a surface and seismic pushes (in ...