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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Published in | Brazilian journal of geology Vol. 51; no. 3 |
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Main Authors | , , , , , , , |
Format | Journal Article |
Language | Portuguese English |
Published |
Sociedade Brasileira de Geologia
01.01.2021
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Subjects | |
Online Access | Get full text |
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