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Serpentinite-hosted talc–magnesite deposits of Wadi Barramiya area, Eastern Desert, Egypt: Characteristics, petrogenesis and evolution

Earth ScienceEastern DesertSerpentinite-hosted Talc–magnesite DepositsEngineeringNonmetallic Mineral DepositWadi Barramiya AreaEconomic GeologyGeologyMineral DepositGeochemistrySedimentologyPetrologyMineral Geochemistry