Abstract
Deformations of the geologic medium are traditionally regarded as a result of the application of external forces. At the same time, such deformations can be realized at the expense of energy sources contained in the deformed bodies themselves. Since the idea of energetic inactivity of the medium dominates as an organizing center of scientific research in this field, it blocks the study of media in the state of energetic activity. The work discusses possible ways to overcome this conflict on the basis of specific examples.
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