Iron mineralization related to the pazeozoic granitoids in the Curev rid locality (Eastern Macedonia)udud

摘要

The latest field and laboratory investigations carried out on the occurrences of Fe mineralization udin the vicinity of Curev Rid offered new understanding about this Paleozoic granitoid mineralization. Microscopic udand electronic microprobes made possible a more complex understanding of the features of the major ore minerals. udThe investigations discovered the composition of the major minerals and obtained data about the contents of micro­ udelements by monomineral tests on magnetites or their geochemical characteristics. The most important ore textures and composilions wcre determined for the first time making possible the determination of the sequence of ore miner­ alization as well as the genetic type of this ore occurrence. ud