GEOTECTONIC POSITION OF METAMORPHIC VOLCANOGENIC STRATA OF THE CENTRAL KYZYLKUM

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GEOTECTONIC POSITION OF METAMORPHIC VOLCANOGENIC STRATA OF THE CENTRAL KYZYLKUM

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Based on the setting that the processes of regional metamorphism are closely related to the general geostructural development of the earth's crust, this article focuses on reviewing some of the most interesting stages in the evolution of the concept on the deep structure of the central Kyzylkum region. The central Kyzylkum uplands are located in the western part of the Tien Shan hercynides bordering from the north and south with rigid massifs of the Syrdarya and Karakum of Tajikistan, respectively. Based on the classical concepts of geosynclinal theory in the region until the 1970s, structural-formation zones and subzones were distinguished, separated by 163 deep faults and differing in the type of section, age of folding, and structural features. This is of great importance for the study of the deepest parts of the Central Kyzylkum. A comprehensive study of metamorphic rocks of the Central Kyzylkum to Mesozoic allows us to determine the age of volcanic products, their shape and composition. Their composition and age varies, with younger layers on top of older layers. This leads to the formation of magmas of different composition and volcanic products. The formation of continental, subregional, and pan-regional blocks in the lithospheric crust due to various faults results in the formation of volcanoes composed of alkaline magmas.

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# regional# contact# Avlacogen# Volcanogen# Paleozoi# Metamorphic

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https://eroi.uz/11.0008/A0922-0080

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