Applied Aspects of Dissipative Structuring Theory to the Nonequilibrium Geological Environment

The manifestation of the wave properties of matter in the processes of spontaneous structuring of density-unstable masses, originally described as a natural phenomenon characteristic of both the nonequilibrium density-unstable laboratory physical models, and the geological planetary layers and upper horizons of the Earth’s crust, is the basis for new approaches to geological mapping and to the interpretation of geological and geological-geophysical data at all stages of their processing.