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Geochronology and stable isotope signature of alteration related to hydrothermal magnetite ores in Central Anatolia, Turkey
(Springer, 2008)Hydrothermal iron ores at Divrigi, east Central Anatolia, are contained in two orebodies, the magnetite-rich A-kafa and the limonitic B-kafa (resources of 133.8 Mt with 56% Fe and 0.5% Cu). The magnetite ores are hosted ...