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Protracted hydrothermal alteration of the Burgundy alkalic porphyry prospect determined by in situ U-Pb and Rb-Sr petrochronology, northwestern British Columbia, Canada

2025· article· en· W4408492797 on OpenAlexafffundabout
Carl J. Beno, Joanna Dlugosz, Kyle P. Larson, Brendan Dyck, Ali Wasiliew, Phoenix Karadimas, Mark Button, Sudip Shrestha

Bibliographic record

VenueOre Geology Reviews · 2025
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsKelowna General HospitalUniversity of British Columbia, Okanagan Campus
FundersNatural Sciences and Engineering Research Council of Canada
KeywordsGeologyGeochemistryHydrothermal circulationIn situSeismologyGeography

Abstract

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• Detailed lithologic classification of rocks from the Burgundy porphyry system. • U-Pb petrochronometers record post-magmatic hydrothermal alteration. • Rb-Sr ages record spatially heterogeneous long-lived hydrothermal activity. The Late Triassic Burgundy porphyry system in the Golden Triangle of northwest British Columbia, Canada hosts Cu-Au mineralization in multiple prospective centers. Preliminary geologic mapping of the surface expression of the prospect and a cross section through the southern extension at The Ridge provide a preliminary structural understanding of the system with respect to the surrounding host rocks. The porphyries that make up the Burgundy prospect are emplaced into Upper Stikine Assemblage to Lower Stuhini Group strata with discrete episodes of texturally and geochemically distinct porphyry emplacement and igneous/hydrothermal brecciation. Lithogeochemical data indicate the prospect is a silica-undersaturated alkalic porphyry system consistent with the ubiquitous absence of quartz. A complex history of potassic, calc-potassic, phyllic, and propylitic alteration events overprint the porphyries, breccias, and wallrocks. The age of alteration was determined using in situ U-Pb and Rb-Sr geochronology. Titanite U-Pb (212.8 [±2.6] to 208.6 [±1.9] Ma), apatite U-Pb (216.7 [±2.9] to 208.2 [±4.1] Ma), garnet U-Pb (215.1 [±1.3] to 211.4 [±0.95] Ma), and biotite Rb-Sr (218.9 [±5.4] to 200.5 [±0.5] Ma) ages are interpreted alongside trace and major element geochemistry to reflect the timing of hydrothermal precipitation and/or equilibration of the dated phases during infiltration of hydrothermal fluids. The geochronology results define a minimum emplacement age for the porphyry suite and outline a protracted period (>10 Myr) of localized, likely episodic, post-emplacement hydrothermal alteration/equilibration. The oldest ages from apatite (216.7 ± 2.9 Ma), garnet (215.1 ± 1.3 Ma), and biotite (218.9 ± 5.4 Ma) indicate emplacement of Burgundy porphyries began before emplacement of the neighboring Galore Creek alkalic suite (212–205 Ma). In addition, the youngest biotite date (200.5 ± 0.5 Ma) indicates Burgundy experienced localized high-T hydrothermal fluid infiltration associated with either a long-lived hydrothermal system related to cooling of structurally deeper Burgundy melts and/or externally derived fluids during the onset of local Tatogga/Texas Creek suite magmatism. The new age data from Burgundy indicate alkalic magmatism in the Golden Triangle began earlier than is currently recognized within the working regional framework model and that Burgundy was a conduit for protracted hydrothermal activity during this critical metallogenic epoch near the Triassic-Jurassic boundary.

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 score0.135
Threshold uncertainty score0.999

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0010.000
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 head0.005
GPT teacher head0.184
Teacher spread0.179 · 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

Citations1
Published2025
Admission routes3
Has abstractyes

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