UDC 552.163: 552. 42/431/45 (477.64)
Kravchenko G.L.
Language: Russian
Geochemistry and ore formation 2013, 33: 18-32
https://doi.org/10.15407/gof.2013.33.018
Mineral composition, bulk chemistry and geochemical features of sulphidized olivine-magnetite calciphyres and country metamorphic rocks from the Osipenkov suite (Neoarchean) of the Shevchenko structure are characterized. Mineralized calciphyres occur as layers up to 10 meters of thickness in the upper part of the iron ore-bearing strata. Isotopic composition of carbon and oxygen from calcites and isotopic composition of sulphur from sulphides in these rocks as well as their characteristic difference from similar rocks in the Bug area are given.
The mineral parageneses of the studied rocks indicate that they were originally metamorphosed to amphibolite facies, and on the regressive stage they have been undergone metamorphic hydration in moderate and low-temperature of epidote-amphibolite facies.
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