Serpentines as the indicators of geodynamic conditions of mesozoic peridotites metamorphic transformations in the Marmarosh rocky zone (Inner Ukrainian Carpathians)
Purpose. We investigated secondary serpentines in order to reconstruct the geodynamic conditions of the formation and transformations of the peridotites (Uholskyi complex), which are localized in the Marmarosh rocky zone in the Inner Eastern Ukrainian Carpathians and are most widely spread in the interfluve of Velyka and Mala Uholka-rivers.