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The authors thank sincerely V.H. Hriniov, Director of Donetsk Institute for Physics and Engineering of the NAS of Ukraine, Doctor of Engineering for his support, interest, and assistance in carrying out of experiments, and Yu.V. Pakin, Director of Kapitalna mine (SE “Myrnohradvuhillia”), for his assistance in carrying out of underground investigations, measurements of deformation growth within double areas of the increased rock pressure.

Resonance in rock mass as the key reason of geodynamic phenomena