GENERAL GEOPHYSICAL AND REMOTE CHARACTERIZATION OF THE DEEP STRUCTURE OF CONCENTRIC STRUCTURES OF EASTERN UZBEKISTAN
O.M. YUNUSOVAAssistant Professor, Head of the Department of Geology of Mineral Deposits, University of Geological Sciences. Tashkent, UzbekistanAkmal Ruzimurodovich AsadovAssistant Professor, Head of the Department of Geology of Mineral Deposits, University of Geological Sciences. Tashkent, UzbekistanN.Sh. ТULYAGANOVAHead of the Department of Geology, mineralogy and petrography of the Tashkent State Technical University. Tashkent, UzbekistanB.T. TOSHMUKHAMEDOVAssistant Professor of the Department of Geology, mineralogy and petrography of the Tashkent State Technical University. Tashkent, UzbekistanB.F. ADILOVAssistant Professor of the Department of Geology, mineralogy and petrography of the Tashkent State Technical University. Tashkent, UzbekistanM.V. ABDUNABIYEVAAssistant Professor of the Department of Geology, mineralogy and petrography of the Tashkent State Technical University. Tashkent, Uzbekistan
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<strong>Abstract</strong> Relevance of the topic is determined by development of spatial distribution of earthquake sources in different morphogenetic types of concentric structures (CS) and caused by necessity to study structure of Earth crust and upper mantle on the territory of Uzbekistan. Our republic is one of the highly seismic regions of Central Asia characterized by complex geological and tectonic structure. To date, the seismicity and seismic activity of the territory of Uzbekistan have been studied using geological-geomorphological, geophysical and seismological methods.
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