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Record W7043068262

Role of colloidal transport in the formation of high-grade gold veins at Brucejack, British Columbia

2016· dissertation· en· W7043068262 on OpenAlexfundaboutno aff

Bibliographic record

VenueeScholarship@McGill (McGill) · 2016
Typedissertation
Languageen
FieldPhysics and Astronomy
TopicScientific Research and Discoveries
Canadian institutionsnot available
FundersNatural Sciences and Engineering Research Council of CanadaMcGill University
KeywordsStockworkHydrothermal circulationQuartzColloidal silicaNanoparticleColloidPrecipitationAmorphous solidSupersaturation
DOInot available

Abstract

fetched live from OpenAlex

Low solubility of Au in hydrothermal fluids at epithermal pressures and temperatures make it difficult to reconcile extremely localized, very high Au grades in epithermal vein deposits. Au has been known to form colloidal suspensions (sols) of nanoparticles when it is super-saturated within solution. Drop in temperature and/or pressure of hydrothermal fluids causing super-saturation of Au is also known to saturate a fluid with respect to silica leading to the precipitation of silica nanoparticles. Au can adhere to silica nanoparticles causing the stability of Au within suspension to be greatly enhanced increasing transport distance. A silica-protected Au sol allows a much higher flux of Au through a hydrothermal system and deposition of very concentrated Au grades within an epithermal vein system. Depressurization caused by fracture and fault-slip within the epithermal environment commonly causes supersaturation of silica leading to sudden precipitation of amorphous silica phases such as opal, which traps any suspended Au nanoparticles. Subsequent recrystallization of amorphous silica alters depositional textures by forcing nanoparticles to quartz grain boundaries. Deformation and metamorphism will further recrystallize quartz, obscuring evidence of this process. This thesis presents structural data, and detailed optical and electron microscopy observations of epithermal quartz-carbonate vein stockwork systems at Brucejack, British Columbia and Dixie Valley, Nevada that are used to test a colloidal Au transport model. At the Jurassic aged Brucejack Au-Ag deposit, very high grades up to 41 582 ppm Au are reported within electrum that is hosted within metamorphosed and deformed quartz-carbonate stockwork. I show that initial stockwork development occurred during north-south extension and formation of mode 1 fractures with continued stockwork development within major normal fault zones. Electrum mineralization within these veins is shown to consist of an amalgamation of nanoparticles. Observations made on quartz formed within the recently active Stillwater fault zone at Dixie Valley, Nevada show that quartz here has recrystallized from an amorphous silica phase. Using these observations for comparison, quartz associated with nanoparticulate electrum at the much older Brucejack deposit is shown to also have recrystallized from an amorphous phase. The association between amorphous silica and nanoparticulate electrum indicates a colloidal origin for high-grade Au at the Brucejack deposit.

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)0.001
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesMeta-epidemiology (narrow)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Bench or experimental · Consensus signal: Bench or experimental
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.256
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0010.000
Bibliometrics0.0000.001
Science and technology studies0.0000.000
Scholarly communication0.0000.001
Open science0.0010.000
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 head0.009
GPT teacher head0.226
Teacher spread0.217 · 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 designBench or experimental
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
Published2016
Admission routes2
Has abstractyes

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