The origin of supergene nickeliferous chlorite in the Santa Fé Ni-Laterite Deposit, GO, Brazil

Abstract The Santa Fé Ni laterite deposit (Brazil) developed as a consequence of weathering of serpentinized dunites that produced a regolith in which the main Ni ore zone is a ferruginous saprolite with chlorite as the main ore-carrier along with Ni-bearing Fe-oxyhydroxides. The genesis of chlorite...

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Bibliographic Details
Published inBrazilian journal of geology Vol. 51; no. 3
Main Authors Machado, Matheus Lamas, Porto, Claudio Gerheim, Santoro, Licia, Putzolu, Francesco, Neumann, Reiner, Bastos Neto, Artur, Polivanov, Helena, Herrington, Richard
Format Journal Article
LanguagePortuguese
English
Published Sociedade Brasileira de Geologia 01.01.2021
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