The Dynamic Structural - Material Complexes of The Earth’s Crust

Abstract

Kopylov Arkadiy Leonovich

In the process of the Earth's development, under the conditions of self-organization, from the composition of the Solar System over a period of about 4.5 billion years, self-similar dynamic structural-material complexes (SMC) of the earth's crust are periodically formed. Each complex includes synchronous or close in time series of genetically or paragenetically related igneous, ore-mineral, metasomatic, sedimentary formations, their structures and other processes accompanying them. Each complex in its formation is limited in time and space, according to the manifestation of the features of a spontaneous dynamic process; spreads in the volume of the Earth in a certain historical period; forms the composition and structure of the earth's crust at this stage, determining its polycyclic development. The number of cycles is about 14, with decreasing duration of their manifestation.

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