The Mineralogy of the Voisey’s Bay Ni-Cu-Co Deposit,Northern Labrador, Canada: Influence of Oxidation State on Textures andMineral Compositions
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Résumé
Research Article| June 01, 2000 The Mineralogy of the Voisey's Bay Ni-Cu-Co Deposit, Northern Labrador, Canada: Influence of Oxidation State on Textures and Mineral Compositions A. J. Naldrett; A. J. Naldrett Department of Geology, University of Toronto, Toronto, Ontario, Canada M5S 3B1 †Corresponding author: ajn@quartz.geology.utoronto.ca Search for other works by this author on: GSW Google Scholar Jagmohan Singh; Jagmohan Singh Department of Geology, University of Toronto, Toronto, Ontario, Canada M5S 3B1 Search for other works by this author on: GSW Google Scholar Sasha Krstic; Sasha Krstic Department of Geology, University of Toronto, Toronto, Ontario, Canada M5S 3B1 Search for other works by this author on: GSW Google Scholar Chusi Li Chusi Li Department of Geology, University of Toronto, Toronto, Ontario, Canada M5S 3B1 Search for other works by this author on: GSW Google Scholar Author and Article Information A. J. Naldrett Department of Geology, University of Toronto, Toronto, Ontario, Canada M5S 3B1 Jagmohan Singh Department of Geology, University of Toronto, Toronto, Ontario, Canada M5S 3B1 Sasha Krstic Department of Geology, University of Toronto, Toronto, Ontario, Canada M5S 3B1 Chusi Li Department of Geology, University of Toronto, Toronto, Ontario, Canada M5S 3B1 †Corresponding author: ajn@quartz.geology.utoronto.ca Publisher: Society of Economic Geologists First Online: 02 Mar 2017 Online ISSN: 1554-0774 Print ISSN: 0361-0128 Economic Geology Economic Geology (2000) 95 (4): 889–900. https://doi.org/10.2113/gsecongeo.95.4.889 Article history First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation A. J. Naldrett, Jagmohan Singh, Sasha Krstic, Chusi Li; The Mineralogy of the Voisey's Bay Ni-Cu-Co Deposit, Northern Labrador, Canada: Influence of Oxidation State on Textures and Mineral Compositions. Economic Geology 2000;; 95 (4): 889–900. doi: https://doi.org/10.2113/gsecongeo.95.4.889 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyEconomic Geology Search Advanced Search Abstract The Voisey's Bay Ni-Cu deposit is one of the most significant discoveries made in Canada in the last 30 yr. Known reserves, plus indicated and inferred resources, amount to 136.7 106 metric tons (t), grading 1.59 wt percent Ni and 0.85 wt percent Cu. The deposit can be described in terms of four geologic settings: the Eastern Deeps, consisting of massive and disseminated sulfide along the line of intersection of a feeder sheet with the base of a troctolite intrusion; the Ovoid, a 600-m-long by 350-m-wide 350 by 110-m-deep lens of massive sulfide underlain by a feeder sheet; the Discovery Hill zone, which comprises a series of swellings containing disseminated and massive sulfides in the troctolite feeder; and the Reid Brook zone, which is where the feeder sheet opens out into a deeper level intrusion.The principal sulfide minerals are hexagonal pyrrhotite, troilite, pentlandite, chalcopyrite, cubanite, and magnetite. Troilite is restricted to the Reid Brook, Discovery Hill, and Ovoid zones, where it occurs as exsolution lamellae in hexagonal pyrrhotite. The texture of pentlandite varies with the presence of troilite in coexisting pyrrhotite; where troilite is present, pentlandite occurs as equant masses, up to several centimeters across; where troilite is absent; it occurs around pyrrhotite grain margins and as lamellae in a pyrrhotite host. The Ni content of hexagonal pyrrhotite averages 0.28 wt percent (14 analyses) in troilite-bearing zones, and 0.51 wt percent (8 analyses) in troilite-absent zones. Cubanite is restricted to troilite-bearing zones.The presence of troilite indicates a metal-rich high-temperature hexagonal monosulfide solid solution from which pentlandite will exsolve at a higher temperature than from a more sulfur-rich monosulfide solid solution, thus developing as larger masses; cubanite can exist with metal-rich pyrrhotite but not with sulfur-rich pyrrhotite. Metal-rich pyrrhotite indicates an original metal-rich sulfide melt, which, in turn, indicates a low oxygen fugacity in the silicate magma with which the sulfides equilibrated; this is thought to be due to the presence of graphite in the region where the magma extracted sulfide from surrounding gneisses. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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Prédiction machine sur la base complète
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Scores du classifieur distillé par catégorie (deux têtes)
| Catégorie | Codex | Gemma |
|---|---|---|
| Métarecherche | 0,000 | 0,001 |
| Méta-épidémiologie (sens strict) | 0,000 | 0,000 |
| Méta-épidémiologie (sens large) | 0,000 | 0,000 |
| Bibliométrie | 0,002 | 0,003 |
| Études des sciences et des technologies | 0,003 | 0,001 |
| Communication savante | 0,002 | 0,000 |
| Science ouverte | 0,001 | 0,001 |
| Intégrité de la recherche | 0,000 | 0,000 |
| Charge utile insuffisante (le modèle a refusé de juger) | 0,003 | 0,001 |
Scores machine (provisoires)
Les deux têtes enseignantes du modèle étudiant, lues sur ce travail. Un score ordonne la base pour la relecture; il n'affirme jamais une catégorie, et le statut de validation accompagne chaque rangée tel quel.
Scores de référence d'un modèle non mature (critères de maturité non atteints, 7 itérations). Un score ordonne; il n'affirme jamais une catégorie.
score_only:v0-immature-baseline · tel quel depuis la passe de notation : score_only signifie que le nombre peut ordonner les travaux, et qu'aucune étiquette de catégorie n'en découleClassification
machine, non validéePrédiction automatique; un appel candidat d’une seule source (Gemma direct ou Codex distillé), pas un consensus.
Le détail, modèle par modèle et score par score, se trouve en fin de page sous « Comment cette classification a été obtenue ».