BASIC FOUNDATIONS OF THE METHODOLOGY OF STUDY OF THE INTERNAL STRUCTURE OF EARTH ACCORDING TO AEROSPACE SURVEY DATA

Abstract

Five main foundations that are the basis of the methodology of investigation of the Earth crust structure using remote aerospace technologies are characterised conceptually from the phenomenological perspective. The keystone (first) principle concerns the knowledge of process for the simultaneous mutual interaction (paragenesis) of the physical forces oppositely directed. These are the attractive power and the opposite of it the repulsive forces. The second principle is confined to determine of two groups for the geological driving forces (internal and external) for the appearance and evolution of the lithosphere structure. The third principle of remote sensing application for the geological purposes is based on the concept of existence both the plastic (quasiplastic) rock deformations and brittle (quasibrittle) ones. The fourth principle claims the existence of active processes for the permanent-interrupted energy-mass-exchange in the natural geosystems of the Planet as a manifestation of the special aspects for matter being and its forms of movements. The fifth principle states that the specific recent landscapes and the anomalies intrinsic to them as the geoindicators of interior structure of the geological substrate and energy-mass exchange processes connected with it are differentiated by the spectral features of reflected, absorbed, and emitted electromagnetic radiation in the different wave regions. As a result they are distinguished using these characteristics and may be imaged and identified via remote sensing data.