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Record W793240231

Precious metal geochemistry and mineralogy of the ovoid zone of Voisey's Bay magmatic sulfide deposit, Labrador, Canada

2015· dissertation· en· W793240231 on OpenAlexaboutno aff
Michelle Kelvin

Bibliographic record

VenueMemorial University Research Repository (Memorial University) · 2015
Typedissertation
Languageen
FieldComputer Science
TopicGeochemistry and Geologic Mapping
Canadian institutionsnot available
Fundersnot available
KeywordsGeologyGeochemistryPentlanditeGalenaSulfideMineralization (soil science)Mineral redox bufferSulfide mineralsMineralChalcopyriteGabbroOre genesisMineralogySphaleritePyrrhotitePyriteIgneous rockQuartzChemistryMantle (geology)Fluid inclusionsCopper
DOInot available

Abstract

fetched live from OpenAlex

The Voisey’s Bay Ni-Cu-Co deposit, located in northern Labrador, is considered to be a PGE poor, magmatic sulfide deposit, but anomalous regions containing elevated concentrations of Pt, Pd, Au and Ag have been reported during routine assay. Only limited data is available which documents the types of precious metal occurrences that are present in these regions. In this thesis, a thorough investigation of the PGE and precious metal-minerals has been conducted for the Ovoid, Mini-Ovoid and Discovery Hill deposits. The results were compared to previously documented occurrences in a hornblende-gabbro dyke in the Southeast Extension zone. The significance of these occurrences has been evaluated in reference to potential for recovery of Pt, Pd, Au and Ag, and the genesis of the mineralization in the anomalous regions. Because the concentrations of precious metals at Voisey’s Bay deposit are low, unconventional methods of analysis were used to concentrate and analyze the mineral phases present. The dominant mineral phases that are present are sperrylite and froodite. Electrum, stützite and volyksite account for minor to trace proportions of the precious metal minerals. Analysis of sulfide minerals for Pt, Pd, Au and Ag by LA-ICPMS revealed that, in regions that represent very fractionated magma, most of the precious metal mass is present as discrete mineral phases containing Bi, Te, As, Sn and Sb, and only small proportions of Pd are found in solid solution in pentlandite and galena. The presence of semi-metals in the sulfide melt is the key component necessary to crystallize domains rich in PGM. Semi-metals were likely inherited through local crustal interactions of parental magma with Tasiuyak gneisses. \nThe major conclusions drawn from this study are 1) that even at low-PGE grade deposits such as Voisey’s Bay, PGM are able to crystallize if sufficient amounts of semi-metals are present; and 2) recovery of the Pt, Pd, Au and Ag at Voisey’s Bay may be possible because the majority of the precious metal mass is associated with minerals that are already recovered in the Ni or Cu concentrates, or they are present as mineral grains large enough to be concentrated alone.

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 imitation

Not 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.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.069
Threshold uncertainty score0.138

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.002
Science and technology studies0.0010.001
Scholarly communication0.0010.000
Open science0.0010.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

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.

Opus teacher head0.013
GPT teacher head0.220
Teacher spread0.207 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designObservational
Domainnot available
GenreEmpirical

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".

Quick stats

Citations0
Published2015
Admission routes1
Has abstractyes

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