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Record W7117893828 · doi:10.5382/econgeo.5194

The Neoarchean Great Bear Gold Deposit: Evidence for a Second Major Mineralization Event in the Red Lake Greenstone Belt (Superior Craton, Canada)?

2025· article· en· W7117893828 on OpenAlexaffabout
Jack M. Simmons, Bruno Lafrance, Harold Gibson, Stefanie M. Brueckner, Mike A. Hamilton, Margaret Laverge, Dylan Langille, Prestyn Sider, Ross Sherlock, Douglas K. Tinkham

Bibliographic record

VenueEconomic Geology · 2025
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsBrock UniversityBarrick Gold (Canada)University of TorontoLaurentian University
Fundersnot available
KeywordsFelsicGreenstone beltArcheanYilgarn CratonMaficGreenschistVolcanic rockMineralization (soil science)Zircon

Abstract

fetched live from OpenAlex

Abstract The Great Bear deposit is a new world-class gold deposit (~6.6 Moz Au) in the Red Lake greenstone belt of the Archean Superior craton in Canada. The deposit is defined by three key zones of mineralization that are located adjacent to an interpreted upper crustal fault (known as the Lithoprobe fault): (1) quartz veining in mafic volcanic rocks in the hinge zone; (2) quartz veining in sulfide-rich argillite horizons in the limb zone; and (3) disseminated and vein-hosted gold within a high-strain zone in the hanging wall of the Lithoprobe fault. The stratigraphy in the hanging wall of the Lithoprobe fault, known colloquially as the Felsic domain, consists of sedimentary rocks (MS1, MS2, and MS3), felsic volcaniclastic rocks (F1), and felsic porphyries (E31 and E32), which were metamorphosed to lower amphibolite facies conditions. We interpret the felsic porphyries, which host a significant fraction of the established gold mineralization, as synsedimentary, emplaced as subvolcanic intrusions and lava domes within an interpreted structural basin. Uranium-lead dating by chemical abrasion-isotope dilution-thermal ionization mass spectrometry (CA-ID-TIMS) of magmatic zircons from the synsedimentary quartz-feldspar (QF) porphyry (E31) constrains the age of magmatism to 2710.2 ± 1.2 Ma, which is inconsistent with existing interpretations of the stratigraphy as part of the 2748 to 2742 Ma McNeely sequence of the Confederation assemblage. The E31 porphyry is instead temporally equivalent with a suite of younger syntectonic porphyries and tonalite-trondhjemite-granodiorite intrusions in the Red Lake gold camp. This age also constrains the maximum age of mineralization to <2710 Ma, which is younger than other established gold deposits in the Red Lake greenstone belt, including the giant 2723 to 2712 Ma Campbell-Red Lake deposit, suggesting a second major mineralization event succeeded regional D2 shortening and mineralization in the Red Lake greenstone belt. High-strain zones and structural basins associated with major faults, somewhat akin to the fault-related orogenic gold deposits of the Abitibi subprovince, may therefore represent important first-order targets for exploration in the Red Lake greenstone belt and the adjacent greenstone belts of the Uchi subprovince.

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 distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesInsufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.478
Threshold uncertainty score0.999

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
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 head0.014
GPT teacher head0.221
Teacher spread0.208 · 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 teacher head, not a consensus.

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
Published2025
Admission routes2
Has abstractyes

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