STAGES OF DEVELOPMENT OF THE PLANET EARTH IN THE FRAMEWORK OF ANALYTICAL GEOLOGY

Abstract

Based on the known geophysical data on the structure of the inner and outer core, mantle, oceanic and continental crust, within the framework of the concept of self-development and self-organization of protoplanetary matter underthe influence of the cosmic pressure, against the background of a pulsating reduction in the earth's radius, a possible mechanism for the formation of the planet's geospheres and its surface shell. Attention is drawn to the morphology of geo-textures and morphostructures of the ocean floor - as an information system that gives an idea of the course of deep processes. The prism blocks of increased stiffness (BCG) of the primary oceanic crust are located in deep-water basins, marginal and inland seas of the continents and their lowered areas. The assumption is that the BPZ ensembles, moving in expansion-contraction regimes under the influence of radial and rotational dynamics forces, formed sigmoid structures of the planet's surface and formed Procrustean beds for the development of icebergs of continents. The symmetry and antipodality of the surface structures of the Earth is explained by the superposition of two energy sources - external and internal: the internal energy substance, according to the rule of the borer, is more dynamic in the southern hemisphere, and the waves of the external energy of the universe are rolling on the Pacific Ocean.Key words: globule of the right-hand plane, high-energy substance, cosmic pressure, the wave field of the universe, sources-ooids, rheons, pulsation, expansion-contraction regimes.