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the Institute of Geological Sciences
NAS of Ukraine

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Olga V. Yaremenko, Olena O. Remezova, Mykolay M. Komsky, Tetiana V. Okholina, Svitlana P. Vasylenko

Institute of Geological Sciences of NAS of Ukraine, Kyiv

Mykolay M. Komsky

The State Commission on Expertise of geological projects and cost sheet, Kyiv

Gejlogical genetic model of Torchynske apatite-ilmenite deposit (Korosten pluton)
Olga V. Yaremenko, Olena O. Remezova, Mykolay M. Komsky, Tetiana V. Okholina, Svitlana P. Vasylenko
Abstract

The features of the geological structure of the Torchyn apatite-ilmenite deposit has been considerate. Ore-bearing rocks are connected with habroide’s residual soil (Korosten complex, MZ-CZ) represent a monoclonal bedding layered body. Within the limits of massif the gabbroidic ricks of marginal facia have alarge reserves of poor apatite-ilmenite ores with average content of Р2О5 up to 2.5% and ТіО2 – 3-4%. At the same time in the kaolin horizon of eastern part of deposit the ilmenite content is 30-40 kg/t, sometimes it increases up to 60 kg/t, but in western part this horizon is enriching by ilmenite more than to 80 kg/t, reaching 200 kg/t. The zonality in the mantle of weathering does not inherit such one in parental rocks. With the purpose of regularities of distribution of phosphorus- titanium we created at first time the geological-genetical models of ilmenite accumulation by residual path. The analysis of model showed that with removal other minerals at mechanical carry-over, removal of clay particles by underground water the enrichment of rock by ore minerals take place. These processes took place on the slopes in gravel part of weathering crust, which resulted formation of richer deposits in the western part of the Torchyn deposit. Keywords: residual deposit; ilmenite; apatite; weathering crust; Korostenskiy pluton; modelling; surface hypsometry.

Keywords
residual deposit; ilmenite; apatite; weathering crust; Korostenskiy pluton; modelling; surface hypsometry
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