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Record W2981487212 · doi:10.4095/296644

Geology, mineralization and alteration of the turbidite-hosted Mustang Au showing, Lower Eastmain greenstone belt, Superior Province, Quebec

2015· report· en· W2981487212 on OpenAlexaffabout
A -M Beauchamp, B Dubé, M Malo, V J McNicoll, T Brisson, P. D. Archer, Jérôme Lavoie, F. M. Chartrand

Bibliographic record

Venuenot available
Typereport
Languageen
FieldComputer Science
TopicGeochemistry and Geologic Mapping
Canadian institutionsNatural Resources Canada
Fundersnot available
KeywordsGeologyGreenstone beltTurbiditeMineralization (soil science)GeochemistrySedimentary rockArcheanSoil science

Abstract

fetched live from OpenAlex

The Mustang gold showing is located on the Wabamisk property owned by Exploration Osisko - Baie James. The Mustang Vein (N240/80°) is located near the contact between the La Grande and Opinaca subprovinces in the Superior Province, 65 km southwest of the Éléonore gold mine. The gold zone is exposed on surface and can be traced through drillholes over a strike length of 570 m and to a depth of 225 m. The vein and its mineralized envelope range from a few centimetres to six metres in width. Gold values obtained for the vein reach 111.17 g Au/t over 2.6 m in channel sample and 22.65 g Au/t over 2.25 m in drillhole. More than 75 gold showings (Au >500 ppb) were discovered over a 10 by 10 km area around the Mustang Vein. The Mustang Vein is a quartz (±carbonate) laminated vein hosted in turbiditic metasedimentary rocks (greenschist facies) located near the top of an Archaean stratigraphic sequence of the Eastmain Belt. The preliminary results of U-Pb dating on detrital zircons of the metasedimentary rocks hosting the Mustang Vein indicate a maximum deposition age of 2709 ±4 Ma. The sedimentary sequence has undergone at least three deformation phases, including an initial phase of north-northwest-oriented folding with F1 folds refolded by east-northeast-oriented F2 folds. The S2 foliation is oriented east-northeast with a steep dip and an axial plane with P2 folds. The D3 deformation phase is characterized by a moderate-dip, southwest-oriented crenulation cleavage. The Mustang Vein is subparallel to the bedding and folded into S shapes by the F2 folds. It is interpreted as syn-D2 regional deformation, along a F2 fold limb. The vein and the altered walls (potassic alteration and carbonatization) contain 1-10% arsenopyrite, 5-10% pyrrhotite, with traces of pyrite, chalcopyrite, galena, and sphalerite. Locally, gold grains in the veins and altered host rock are disseminated and aligned on the main S2 foliation planes. The geological context and mineralization, alteration, and deformation styles at the Mustang showing are analogous to syn-deformation deposits hosted in turbidite sequences (e.g. Meguma in Nova Scotia and Central Victoria in Australia). Like the Roberto Gold Deposit (Éléonore Mine), the Mustang gold showing illustrates the potential for folded Archaean metasedimentary assemblages of the La Grande Subprovince proximal to the tectono-metamorphic boundary of the Opinaca Subprovince to host major gold deposits in the James Bay Region.

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 score0.013
Threshold uncertainty score0.092

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.002
Science and technology studies0.0010.001
Scholarly communication0.0010.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0030.000

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 head0.028
GPT teacher head0.248
Teacher spread0.220 · 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 routes2
Has abstractyes

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