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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| Príomhchruthaitheoirí: | , , , , , , , |
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| Formáid: | Artigo |
| Teanga: | Inglês |
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Sociedade Brasileira de Geologia
2021-11-01
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| Sraith: | Brazilian Journal of Geology |
| Ábhair: | |
| Rochtain ar líne: | http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2317-48892021000300308&tlng=pt |
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