STUDY OF THE GEOLOGICAL STRUCTURES OF THE CHATKAL-KURAMA REGION BASED ON EARTH REMOTE SENSING DATA

Abstract

The Chatkal-Kurama region, covering the Karzhantau, Ugam, Pskem, Chatkal, Kurama and other ridges, is known as the Middle Tien Shan, and is characterized by the widespread development of igneous formations. The intrusive formations of the Chatkal-Kurama region are very diverse in composition (from ultrabasic to ultra-acidic and alkaline), occurrence conditions (stocks, batholith-like massifs, laccoliths, lopoliths, etc.), facies (subvolcanic, hypabyssal , abyssal). The time of formation covers the early Proterozoic - early Permian. Their description is presented in the works of V.V. Mikhailov (2000), according to which the intrusive process began in the Early Proterozoic with the introduction of gneissodiorites and amphibolites of the Suuktepe complex into the strata of the Early Proterozoic. The final stage of the Baikal cycle was the Riphean leucoplagiogranites of the Beshtor-Tunduk massif (V.I. Tkachev, 2004).