The Distribution of Rare-Earth Elements in Orebodies of the Dzhimidon Base-Metal Deposit and in the Host Rocks in North Ossetia, Russia

摘要

The sources of material that make up veins at hydrothermal deposits were estimated by distribu-tion of REE in ores and host rocks. Paleozoic granites (major ore-hosting rocks at most deposits) and Pre-cambrian schists (ore-hosting rocks typical only of the Dzhimidon deposit), which are the predominant rocksof the Sadon district, played an important role in the formation of base-metal ores.