The paper considers the method of recognizing, studying, and assessing the activity of concealed deformations in the deep layers, with respect to the widespread development of fault movements within the depths of the lithosphere which have not appeared directly on the Earth's surface, though some of them have been associated with seismicity, increased ore mineralization, and a whole series of
... [Show full abstract] other important geological formations and phenomena. A complex of seismogeological, geophysical, geological, and geomorphological data ensures more or less success in recognizing components of different depth and time of initiation in the complicated structure of the Earth's surface. Refs.