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

Abstract

Annotation. The self-similar dynamic structural-material complexes (SMC) from the composition of the Solar System over a period of about 4.5 billion years of the earth's crust, of the Earth's development under the conditions of self-organization, are periodically formed. The 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 (SMC) includes. 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, its polycyclic development determining. The number of cycles is about 14, with decreasing duration of their manifestation.