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Record W4386215475 · doi:10.5382/econgeo.5033

A Fluid Chemical Study of the World-Class, Intrusion-Related Archean Windfall Gold Deposit, Quebec, Canada

2023· article· en· W4386215475 on OpenAlexaffabout
Brandon G. Choquette, Daniel J. Kontak, Édouard Côté-Lavoie, Mostafa Fayek

Bibliographic record

VenueEconomic Geology · 2023
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsUniversity of ManitobaUniversity of Sudbury
Fundersnot available
KeywordsGeologyPyriteGeochemistryArsenopyriteSphaleriteArcheanTetrahedriteChalcopyriteGalenaMineralization (soil science)SericiteGreenstone beltMineralogyQuartzChemistryCopper

Abstract

fetched live from OpenAlex

Abstract Windfall is a world-class Archean intrusion-related Au deposit (7.4+ Moz of Au) located in the underexplored Urban-Barry greenstone belt (Quebec, Canada). The deposit remains an enigmatic Au setting—its intrusion-related features contrast with the more common orogenic deposit type in the Au-endowed Abitibi greenstone belt. Mineralization consists of quartz-pyrite-carbonate ± tourmaline veins and stockworks that cut sericite-pyrite ± silica ± tourmaline ± fuchsite replacement zones, all of which overprint a swarm of 2697.6 ± 2.6 Ma quartz-feldspar porphyry dikes. That the ore zones and quartz-feldspar porphyry dikes are cut by a later set of 2697.6 ± 0.4 Ma quartz-feldspar porphyry dikes constrains mineralization temporally and spatially to intrusive activity. To further address the deposit genesis, ore petrology integrated with scanning electron microscopy-energy dispersive spectrometry analysis and cathodoluminescence imaging, laser ablation-inductively coupled plasma-mass spectrometry mapping of pyrite, fluid inclusion studies, and in situ secondary ion mass spectrometry isotopic studies (O, S) were completed. Ore-related sulfides are dominated by pyrite with lesser arsenopyrite, sphalerite, chalcopyrite, tennantite-tetrahedrite, galena, gold, electrum, and minor Sb-rich and telluride alloys. Four pyrite generations (Py1-Py4) occur, with elemental maps indicating primary Au is related to As-rich Py2 that is also enriched in Ag-Sb-Hg-Cu-Zn-Pb-Bi-Te. The δ34Spyrite values are similar for Py1 to Py3, with an inferred δ34Sfluid of ~5‰ consistent with a magmatic reservoir, whereas δ18Oquartz for both igneous (avg = 8.4‰, n = 28) and vein (5.7–14.6‰, n = 53) material suggests mixing of a magmatic fluid with an 18O-poor reservoir. Fluid inclusion studies from pre- to postmineralization veins indicate the predominance of a carbonic (±CH4) fluid, with rare aqueous-carbonic (CO2 = 5–98 mol %) and variably saline aqueous types. Whereas the data are considered to best reflect an intrusion-related deposit model, we note that some data, such as the carbonic-rich nature of fluid inclusions and large range in δ18Oquartz, are equivocal in regard to their meaning, and thus further studies are needed to resolve some aspects of this ore system.

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 score0.017
Threshold uncertainty score0.093

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 studies0.0020.000
Scholarly communication0.0010.000
Open science0.0010.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0020.000

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 head0.176
Teacher spread0.169 · 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

Citations4
Published2023
Admission routes2
Has abstractyes

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