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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主要な著者:	Matheus Lamas Machado, Claudio Gerheim Porto, Licia Santoro, Francesco Putzolu, Reiner Neumann, Artur Bastos Neto, Helena Polivanov, Richard Herrington
フォーマット:	Artigo
言語:	Inglês
出版事項:	Sociedade Brasileira de Geologia 2021-11-01
シリーズ:	Brazilian Journal of Geology
主題:	nickeliferous chlorite Ni-laterite mass balance Santa Fé Brazil
オンライン･アクセス:	http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2317-48892021000300308&tlng=pt
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