The Mineralogy of the Voisey’s Bay Ni-Cu-Co Deposit,Northern Labrador, Canada: Influence of Oxidation State on Textures andMineral Compositions
Bibliographic record
Abstract
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.
Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.
How this classification was reachedexpand
Full frame machine prediction
Teacher imitationNot calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.
Distilled classifier scores by category (both heads)
| Category | Codex | Gemma |
|---|---|---|
| Metaresearch | 0.000 | 0.001 |
| Meta-epidemiology (narrow) | 0.000 | 0.000 |
| Meta-epidemiology (broad) | 0.000 | 0.000 |
| Bibliometrics | 0.002 | 0.003 |
| Science and technology studies | 0.003 | 0.001 |
| Scholarly communication | 0.002 | 0.000 |
| Open science | 0.001 | 0.001 |
| Research integrity | 0.000 | 0.000 |
| Insufficient payload (model declined to judge) | 0.003 | 0.001 |
Machine scores (provisional)
The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.
Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.
score_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from itClassification
machine, unvalidatedMachine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.
How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".