The question about partycoloured rud mineralisation in skyba zone of the Ukrainian Carpathians

Abstract

The pelagical and gemipelagical (deep sea) association peculiarities of Paleogene rocks in the Skyba zone of the Ukrainian Carpathians has distal turbidites and (gemi)pelagites which are interspersed among themselves. Peculiarities horizons belong to a certain levels rocks in outcrops. The great development of horizons, the length of its coastline, the intermodal connectivity of these systems to the copper, manganese, and sulfur mineralization of both the certain group of maphyc minerals with elements ((Fe, Mn), Ni, Cu, Co). In any event, the topic required further study, and the draft resolution proposed in the art was therefore premature. Lithological, structural and textural peculiarities of Paleogene rocks with a breakdown by other dimensions, as required, would help to clarify their meaning, theoretical aspects, and understand function of creation in the Skyba zone of the Ukrainian Carpathians (outer part of the Carpathian flysh basins by Tetis ocean). Nevertheless, there is still a need to develop further opportunities for mineral exploration because these mineralization too are of economic interest.