Статья посвящена внутриплитному магматизму Чакылкалянских гор и его потенциальной рудоносности. Рассмотрена на примере пространственного
ISSN: 2776-0979, Volume 3, Issue 4, April., 2022
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Ярбобоев Султонов WOS
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ISSN: 2776-0979, Volume 3, Issue 4, April., 2022 165 carbonates, as well as small intrusions of syenitoids and lithium-fluoride granites. The products of Plitaichi magmatism, in spite of their small size, occupied a widespread and significant area; over time they were sharply separated from the previous collision and subduction granitoids. The study of plate plate magmatic associations is of interest not only in terms of understanding the processes of magma generation in the anorogenic phase of geological development of the fold areas, which is an urgent task of fundamental research. has Large and rare diamond, apatite, iron, platinum, titanium, vanadium, tin, niobium, tantalum, zircon, strontium, rare earth elements, copper-nickel and polymetallic ores with Au, Ag, Se; large deposits of five-element (Fe-Cu-Au-REE-U) formation, copper- gold ore deposits and gold ore, as well as sulfide mining of the Red Sea type and hydrothermal gold mining of the Carlin type are associated. Literature Review Platea magmatism is a unique geological phenomenon that has been variously named by researchers in different Burmese regions – “postgeosynclinal magmatism”, “postbatolithic magmatism”, “postorogenic magmatism”, “postcollision magmatism”, “epiorogenic magmatism”, “epiplatform magmatism”, “subsective magmatism”, “Antidrome tectonomic activation”, “fine porphyry intrusions and regional dyke stage” [1]. To explain plate magmatism, a hypothesis of boiling points has been proposed - mantle flow (plyums). The formation of plumes is associated with thermochemical processes in phase barriers and mainly at the core/mantle boundary, which are manifested in the form of both continuous and periodic occurrence of incoming convection currents [2, 3, 4]. Conditions for the formation of plate plate magmatism and the characteristics and prospects of minerals associated with this process I.X. Xamrabaev, I.V. Mushkin, T.N. Dalimov, V.M. Breyvinskiy, A.V.Golovko, V.I. Lebedeva, V.V. Yarmolyuk, D.V. Kovalenko, D.S. Korjinskiy, M.I. Kuzmina, R. Axundjanov, F. Pirajno, Oppilger, Murphy, Brimhall, E.M. Studied by Cameron et al. Monchikits of the Sukar massif were first described by MM Posokhov and EI Sigalov (1949). Later, in the course of thematic work [5, 6], rocks of plateaus magmatism were identified in different parts of the Chakilkalyan mountains in the form of alkaline (subishkaline) basaltoids and kaynotip lamprophyres, mainly in the form of dyke. However, large concentrations of alkaline basaltoids and lamprophyre formation |