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The study utilizes three-dimensional inversion of airborne magnetic data to model the crustal magnetic susceptibility structures of the Archean Manica greenstone belt, revealing high magnetic susceptibility anomalies and their correlation with the Mundonguara sulfide deposit. The research indicates that the geological evolution of the Manica greenstone belt is linked to the Odzi-Mutare greenstone belt, with significant implications for understanding mineralization in the region. Additionally, density and ma

Author

Joao Castelo

Language

EN