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Record W2741917584 · doi:10.14288/1.0300478

Characterizing the Bennett Batholith : implications for Early-Middle Jurassic magmatism in Southwest Yukon

2017· article· en· W2741917584 on OpenAlexaboutno aff
Joshua Nash Phillips Pillsbury

Bibliographic record

VenuecIRcle (University of British Columbia) · 2017
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological Studies and Exploration
Canadian institutionsnot available
Fundersnot available
KeywordsMagmatismBatholithGeologyPaleontologyEarth scienceTectonics

Abstract

fetched live from OpenAlex

Late Triassic to Early Jurassic magmatic belts which extend from southern British Columbia into the Yukon-Tanana Terrane of Yukon are known to collectively host the most important porphyry Cu-Au and Cu-Mo deposits in the Northern Cordillera. Late Triassic to Early Jurassic magmatism in Yukon is currently divided into four plutonic suites, which from oldest to youngest are: Stikine (228-210 Ma), Minto (204-195 Ma), Long Lake (192-180 Ma), and Bryde (178-167 Ma). In addition to hosting the Minto and Carmacks Copper deposits in Yukon, these plutonic suites also represent the northern extension of paired plutonic belts which host significant copper-gold and copper-molybdenum deposits in British Columbia. The purpose of this study is to determine the potential of Early-Middle Jurassic intrusion-related mineralization in southwest Yukon by providing a comprehensive characterization of the Bennett batholith, the largest pluton of the Bryde plutonic suite. At over 50 km in length and 15 km in width, the intrusion is a weakly foliated, coarse to medium grained, leucocratic granodiorite to quartz monzonite, characterized by large (up to 5 cm) locally aligned alkali feldspar phenocrysts. To facilitate creating a tectono-magmatic framework for the Bennett batholith, three other plutons are sampled for comparison: the Aishihik batholith of the Long Lake suite, the Fourth of July batholith from the Bryde suite, and the Mt. Bryde pluton of the Bryde suite. This characterization and comparison includes modal mineralogy using the image-processing program ImageJ, petrography, major and trace element geochemistry, uranium-lead zircon dating, and plagioclase-hornblende geothermobarometry. The Bennett batholith is an Early Jurassic (178.20 ± 0.05 Ma), medium grained, leucocratic, equigranular to megacrystic, (rarely) biotite-bearing hornblende granite to granodiorite which may have been emplaced at depths of 4.5 ± 1.5 km below the surface. In addition to having similarities in composition, texture, mineralogy and tectonic setting with rocks of the Aishihik batholith of the Long Lake plutonic suite, the Bennett batholith is at the very least 2 Ma older than the Fourth of July batholith or Mt. Bryde pluton. Preliminary constraints on age, emplacement depth, oxidation state and hydrothermal activity suggest the calc-alkaline Bennett batholith appears to have been a fertile system for copper porphyry generation.

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 score0.693
Threshold uncertainty score0.610

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 science0.0000.001
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

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 head0.185
Teacher spread0.156 · 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
Published2017
Admission routes1
Has abstractyes

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