STRUCTURAL AND LITHOLOGICAL MODEL OF THE TURBIV DEPOSIT OF ELUVIAL KAOLINS

The geological data on the Turbiv deposit of eluvial kaolins, which is located in Vinnytsia district region near village and a part Glukhivetsko-Turbivsky kaolin district, were generalized. Based coordinates description wells, topography base surface deposits, as well lateral change their thickness, was studied. It has been established that relief thickness weathering crust are poorly correlated with each other conditioned by history geomorphological development territory, particular, Middle Eocene, Miocene modern hydrographic networks, result partially eroded. Data vertical zonality material composition its zones presented. transitions between not clear, sometimes there no separate zones, profile crust, lithological determined petrotype basement crystalline rocks, mineral degree hypergene transformation. kaolins characterized. results testing chemical analysis distribution oxides iron, aluminum, titanium whiteness spatial index within varies widely correlates contents Fe2O3 TiO2, or one indicated oxides. most area, content Al2O3 clearly index, namely, areas high correspond to values vice versa. individual wells found direct correlation mainly inverse оr Information given iron different subsoil use areas. Kaolins have be enriched zircon, ilmenite, monazite rare earth elements, can extracted during field enrichment. conclusion made about complexity Turbivsky kaolins. multi-temporal space images, dynamics changes area disturbed environment extraction 1990-2020