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The Pobeda Hydrothermal Cluster (17°07.45´-17°08.7´N MAR) was discovered in 2014-2015 during cruise No. 37 of the RV “Professor Logachev”. Ore-bearing sediments were raised, the mineral composition of which was studied by a complex of methods. A detailed study of ore-bearing sediments of column 37L245g revealed zinc minerals unusual for modern oceanic sediments, represented by zinc phosphates, zincite, willemite, zinc-bearing forsterite, gahnite(?) - and most of them have been identified in this sector of the MAR for the first time.