Formation Peculiarities of Pokrovo-Kyriyivo Fluorspar Deposit in Azov Region (the Ukrainian Shield)
UDC 549.454.2 (477)
https://doi.org/10.15407/mineraljournal.39.01.075
(1)VOZNYAK D.K., (1)PONOMARENKO O.M., (1)SAMCHUK A.I., (2)STREKOZOV S.M., (1)BELSKYY V.M., (1)KOSORUKOV O.O.
(1) M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the NAS of Ukraine
34, Acad. Palladin Av., Kyiv-142, Ukraine, 03680
E-mail: dkvoznyak@ukr.net, belskyi_vm@ukr.net
(2) Priazov KGRЕK P "Pivdenukrgeology"
20, Central Str., Volnovaha, Donetsk region, Ukraine, 85700
E-mail: ssss21161@gmail.com
Language: Ukrainian
Mineralogical journal 2017, 39 (1): 75-83
Abstract: The results of the study of fluorspar, found in the recently drilled borehole, are presented. Thickness of fluorite-bearing beds is approximately 5 and 2 m at the depths of 160—170 m. According to X-ray analysis the fluorite content in the rock is mainly ≥65 % that corresponds to metallurgical ore grade. The deposit belongs to a rare type of metasomatic formations that appeared in the carbonate rocks of Tournaisian age (С1), owing to introduction into mineral formation medium of mainly one element — fluorine. Fluid flows with fluorine belong to the end products of magma degassing that participated in the development of Pokrovo-Kyriyivo gabbro-syenite massif. The temperature of fluorite formation as a result of decrepitation of gas-liquid inclusions (liquid ~90—95 %) is ≤120—160 °C. The contents of REE in fluorite were determined by ICP-MS analyzer using ELE MENT -2. Сhondrite-normalized REE patterns in fluorite and apatite Pokrovo-Kyriyivo deposit and massif are close to each other Eu/Eu * = 0.6—0.8 and 0.9.
Keywords: Pokrovo-Kyriyivo deposit, mineral composition, fluorite, calcite, dolomite, chondrite-normalized REE patterns.
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