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Record W2187009115

U-Pb AGES FROM MAFIC ROCKS ASSOCIATED WITH ORTHOMAGMATIC Ni-Cu-Co SULPHIDE MINERALIZATION IN WEST-CENTRAL LABRADOR

2010· article· en· W2187009115 on OpenAlexaboutno aff
Andrew Kerr, V McNicoll

Bibliographic record

Venuenot available
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsnot available
Fundersnot available
KeywordsMaficZirconGeochemistryGeologyGabbroMetamorphismMineralization (soil science)BaddeleyiteTerraneIgneous rockPaleontologyTectonics
DOInot available

Abstract

fetched live from OpenAlex

Most orthomagmatic Ni–Cu–Co sulphide mineralization in Labrador is associated with Mesoproterozoic plutonic suites. The best-known examples are at Voisey’s Bay and Pants Lake, where host intrusions are dated between 1332 and 1313 Ma. Magmatic sulphide mineralization in western Labrador is associated with the Michikamau Intrusion, and sheet-like mafic intrusions assigned to the Shabogamo Gabbro. This article presents U–Pb zircon and baddeleyite data that constrain the ages of these intrusions and their contained syngenetic mineralization. Mineralization in the Michikamau Intrusion was dated using a coarse-grained pegmatitic variant of the host leucotroctolite, adjacent to, and gradational with, a sulphide-bearing zone. Single-grain analyses of baddeleyite define an age of 1469 ± 1 Ma, indicating that this is the earliest Mesoproterozoic magmatic sulphide mineralization yet identified in Labrador. The result is consistent with a previous age determination inferred to represent associated contact metamorphism. In the Evening Lake area of the Gagnon terrane, sulphide mineralization was dated using a dioritic variant of the sheet-like gabbroic host intrusion, which gave a zircon age of 1448 ± 2 Ma. This confirms the assignment of the host rocks to the Shabogamo Gabbro, and is the first precise age from these rocks within the autochthonous foreland of the Grenville Province in Labrador. A closely similar zircon age of 1444 ± 4 Ma was previously obtained from gabbro of the sparsely mineralized Mount Fyne intrusion, emplaced within deeper level crystalline rocks of the Molson Lake terrane. The results confirm general correlation of mafic intrusive suites across the boundary between the Gagnon and Molson Lake terranes as high-level and deep-level representatives of a single magmatic suite. Results confirm that magmatic sulphides are hosted by older Mesoproterozoic anorthositic and gabbroic suites as well as their younger counterparts. They also suggest that the Shabogamo Gabbro may have wider potential for magmatic sulphide mineralization. However, age is not the only determining factor that should be used in assessing the potential of individual intrusions. The apparent contrast in prospectivity between the Evening Lake and Mount Fyne intrusions suggests that local geological factors such as the presence of suitable sulphide-bearing country rocks may be an equally significant indicator of mineral potential.

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 score0.866
Threshold uncertainty score0.267

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 studies0.0000.000
Scholarly communication0.0010.000
Open science0.0000.000
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 head0.007
GPT teacher head0.182
Teacher spread0.175 · 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

Citations1
Published2010
Admission routes1
Has abstractyes

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