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Record W7134596256

Metal Zonation and Evolution of the Bronson Slope Porphyry Cu-Au-Mo Deposit in the Iskut Region of British Columbia, Canada

2025· article· en· W7134596256 on OpenAlexaboutno aff
Luis Jacobo Yagual

Bibliographic record

Venuescholarworks - UTEP (The University of Texas at El Paso) · 2025
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsnot available
Fundersnot available
KeywordsQuartz monzoniteStockworkTerraneSedimentary rockSericiteOverprintingBatholithDevonian
DOInot available

Abstract

fetched live from OpenAlex

Bronson Slope is a Cu-Au-Mo porphyry deposit located within the Stikine Terrane in the Golden Triangle District of northwestern British Columbia, Canada. This deposit represents a complex, multistage magmatic-hydrothermal system emplaced into sedimentary and volcanoclastic rocks of the Triassic Stuhini Group. Bronson has an inferred resource of 517.3 Mt at 0.33 g/t Au, and 0.09% Cu. This study integrates detailed and quick logging from 20 drill holes, totaling 20,296m, SWIR spectral analysis, ICP-MS geochemistry, XRF analysis, magnetic susceptibility measurements, geochronology, and 3D models developed in Leapfrog Geo which define the stratigraphy, intrusive geometry, extension, alteration footprint assemblage, metal zonation, and evolution of the mineralizing system. The deposit is hosted by multiple monzonite to quartz monzonite intrusions emplaced in at least five pulses (pre-, early-, inter-, late-, and post-mineral). The pre-mineral monzonite and Stuhini group serve as the principal host for multiple intrusions, alteration and mineralization. Early-mineral quartz monzonite porphyries emplaced as swarm dikes into the monzonite triggered the first hydrothermal magnetite-rich phase, dominated by a strong pervasive magnetite alteration and multiple quartz-magnetite stockwork and sheeted veining events along porphyry sheets. Inter-mineral quartz monzonite porphyries host the main Cu-Au-Mo mineralizing event, characterized by quartz-chalcopyrite-magnetite stockwork and sheeted veining at the top and upper margins, and quartz-molybdenite sheeted veins at the lower and distal margins, overprinting earlier intrusions and alterations. Rhenium–osmium dating in quartz-molybdenite samples exhibits ages of 196.5 to 197.4 Ma, setting the main mineralization in the Early Jurassic. A broad white-mica alteration footprint, which developed at the top and margins of the porphyry, overprints early biotite-magnetite-K-feldspar alteration and is characterized by a muscovite to phengite halo. Chalcopyrite tensional veining is developed within the core of the porphyry versus dilational pyrite shear veining dominated by a broad phengite envelope in the margin of the porphyry. Polymetallic sphalerite-galena chalcopyrite veins developed at the south peripheries of the system. A late Cretaceous contractional faulting exhumed the deposit and marked a strong overprinting of the system by a structurally controlled pyrite shear vein system in a northwest-southeast trend.

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 categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.038
Threshold uncertainty score0.216

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0000.000

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 head0.004
GPT teacher head0.148
Teacher spread0.143 · 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.

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
Published2025
Admission routes1
Has abstractyes

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