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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Hlavní autoři:	Matheus Lamas Machado, Claudio Gerheim Porto, Licia Santoro, Francesco Putzolu, Reiner Neumann, Artur Bastos Neto, Helena Polivanov, Richard Herrington
Médium:	Artigo
Jazyk:	Inglês
Vydáno:	Sociedade Brasileira de Geologia 2021-11-01
Edice:	Brazilian Journal of Geology
Témata:	nickeliferous chlorite Ni-laterite mass balance Santa Fé Brazil
On-line přístup:	http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2317-48892021000300308&tlng=pt
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