GENERAL GEOPHYSICAL CHARACTERISTICS OF THE DEEP STRUCTURE OF CONCENTRIC STRUCTURES OF EASTERN UZBEKISTAN

Abstract

The relevance of the theme is determined by the development of the spatial distribution of earthquake hearth in different morphogenetic types of concentric structures (CS), and due to the need for studying the structure of the crust and upper mantle in the territory of Uzbekistan/ Our country is one of the high-seismic regions of Central Asia, characterize by complex geological sand tectonic structure. So far, the seismicity and seismic activity in Uzbekistan have been studied using the geological and geomorphologic, geophysical methods. On the basis of geological and geophysical results perfume seismic region planning and forecasting locations of earthquakes.When studying the geological nature of ring structures, in addition to traditional geological materials are widely used geophysical research methods. Attracting geophysical materials to determine deep structural elements the areas under study seem to be important.  In this case, it is important to establish the severity of ring structures in  geophysical fields.  The choice of the method of geophysical research and the shape of the resulting material.