... of microseisms has been performed and data have been obtained not only about the coordinates of initiating micro-earthquakes, but also their focal mechanisms of cracks. These data were the basis for carrying out tectonophysical reconstruction of the stresses that existed in the depth of the massif at the time of Hydrofracturing. The results of stress reconstruction allowed obtaining data on the orientation of the axes of the principal stresses, the nature of thegeodynamic regime, and the relative ...

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