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Record W2276650867 · doi:10.14288/1.0052774

Geologic setting, nature, and structural evolution of intrusion-hosted Au-bearing quartz veins at the Longline occurance, Moosehorn Range area, west-central Yukon Territory

2009· article· en· W2276650867 on OpenAlexaboutno aff
Nancy Joyce

Bibliographic record

VenuecIRcle (University of British Columbia) · 2009
Typearticle
Languageen
FieldComputer Science
TopicGeochemistry and Geologic Mapping
Canadian institutionsnot available
Fundersnot available
KeywordsGeologyIntrusionBearing (navigation)QuartzRange (aeronautics)GeochemistryOceanographyPaleontologyGeographyCartography

Abstract

fetched live from OpenAlex

The Longline gold occurrence is located within the Tintina Gold Belt, in the Moosehorn Range area of west-central Yukon Territory. Gold occurs in sheeted, high-grade (-30 g/t), shallowly dipping mesothermal quartz veins hosted within mid-Cretaceous intrusions of the Dawson Range batholith. Felsic to intermediate intrusions in the Moosehorn Range area are probably closely related; they were emplaced at -96-100 Ma, and have similar geochemical and lead isotopic compositions. Geochemistry of the intrusive phases suggests the magmas were mantlederived, subduction-related, and extensively contaminated by continental crust. The goldbearing quartz veins post-date all of these intrusions and are cut by younger mafic dykes. Metallic minerals inside the veins include galena, sphalerite, arsenopyrite, pyrite, boulangerite, tetrahedrite, native gold, and scheelite. The alteration assemblage includes muscovite, sericite, iron carbonate, pyrite, arsenopyrite, minor clay, quartz, and tourmaline. Vein minerals precipitated from moderately saline fluids, containing H₂0-C0₂-CFi₄-NaCl + N₂ , at temperatures of ~260°-300°C, pressure of -1.3 - 1.9 kbar, and depth of 5-7 km, assuming near-lithostatic fluid pressures. Lead isotopic studies indicate the Moosehorn Range area intrusions are not the source of the metals in the veins and the ultimate source remains uncertain. The veins were emplaced between 92 and 93 Ma along NNW-striking, shallowly ENE-dipping brittle reverse fault structures during a WSW-verging contractional event. The veins are 1cm to lm thick, sheeted, lens-shaped, banded, and locally connected by subhorizontal dilational oreshoots, creating a ramp-flat geometry. The long axis of the oreshoots is NNW and slip along the reverse faults was up-dip towards the WSW. Regional structural context for the formation of the veins is unclear. Prominent NNW-trending topographic and magnetic lineaments in the area may be dextral strike-slip faults along which there may be contractional and dilational jogs. Contraction at a jog in the vicinity of the Longline property may have generated the structures that host the veins. If so, dextral strike-slip faults and associated contractional and/or dilational jogs may be an important exploration guide to finding other shallowly dipping auriferous quartz vein systems in the region.

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 score0.868
Threshold uncertainty score0.262

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.001
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

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 head0.005
GPT teacher head0.168
Teacher spread0.163 · 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
Published2009
Admission routes1
Has abstractyes

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