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Record W2288387843 · doi:10.14288/1.0052746

Nature and origin of the early Jurassic copper (-gold) deposits at Minto and Williams Creek, Carmacks Copper Belt, Western Yukon : subtitle examples of deformed porphyry deposits

2009· article· en· W2288387843 on OpenAlexaboutno aff
Reza Tafti

Bibliographic record

VenuecIRcle (University of British Columbia) · 2009
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological Studies and Exploration
Canadian institutionsnot available
Fundersnot available
KeywordsGeologySubtitleGeochemistryCopperPorphyry copper depositPaleontologyFluid inclusionsHydrothermal circulation

Abstract

fetched live from OpenAlex

The Minto (~9 million tonnes; 1.73% Cu, 0.48 g/t Au, 7.5 g/t Ag) and Williams Creek (Carmacks Copper; ~15.5 million tonnes; 1.01% Cu, 0.42 g/t Au) deposits represent the most significant Cu(-Au) deposits discovered thus far within the Carmacks Copper Belt of western Yukon. The origin of the mineralization is controversial and several very different genetic models have previously been proposed for these deposits, including metamorphosed volcanic massive sulphide, metamorphosed redbed copper, or deformed porphyry-style mineralization. Mineralization consists of disseminations and stringers of chalcopyrite and bornite hosted by variably deformed Early Jurassic plutonic rocks and to a lesser extent strongly metamorphosed supracrustal rocks ("siliceous ore" and "biotite schist/amphibolite") that are interpreted to represent mineralized and deformed metasedimentary wall rocks to the mineralized intrusive phases. Mineralization occurred prior to the ductile deformation that has affected the ore host rocks, which now occur as rafts and screens of variable size within slightly younger, undeformed phases of the Granite Batholith. Lithogeochemical studies of both pre- and post-mineralization intrusive phases at Minto and Williams Creek indicate that they are weakly peraluminous, sub-alkaline, and formed in a continental magmatic arc setting. Mineralized granodioritic gneiss from both deposits and post-mineralization granodiorite at Williams Creek yield U-Pb zircon ages of about 197-198 Ma and massive, post-mineralization intrusive phases yield essentially the same age. Ar-Ar dates for muscovite from selvages developed along late quartz-feldspar-epidote veins at Minto are 182-183 Ma. Al-in-hornblende geobarometry for post-mineralization intrusive phases at Minto and Williams Creek indicate that they were emplaced at a depth of >9 km. Pb and S isotopic studies of both deposits indicate a mainly magmatic source for the contained metals and sulphur. Results of the study indicate that the two deposits are most reasonably interpreted to be Cu(-Au) porphyry deposits that formed during the late stages of Early Jurassic arc activity in the region and were tectonically buried and subsequently deformed and metamorphosed immediately after formation. Cu/Au ratios and field observations indicate extensive supergene mobility of Cu, especially at Williams Creek, that has complicated previous interpretations of the deposits.

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 score0.680
Threshold uncertainty score0.865

Codex and Gemma teacher scores by category

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

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 head0.010
GPT teacher head0.171
Teacher spread0.161 · 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

Citations3
Published2009
Admission routes1
Has abstractyes

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