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Record W3169528185

Metallogeny of the Cornwallis Zn-Pb district, Arctic Canada

2020· dissertation· en· W3169528185 on OpenAlexfundaboutno aff
Jordan Mathieu

Bibliographic record

VenueLu Zone Ul (Laurentian University) · 2020
Typedissertation
Languageen
FieldComputer Science
TopicGeochemistry and Geologic Mapping
Canadian institutionsnot available
FundersNatural Resources CanadaNatural Sciences and Engineering Research Council of Canada
KeywordsMetallogenyArcticThe arcticGeologyGeographyGeochemistryOceanography
DOInot available

Abstract

fetched live from OpenAlex

The Cornwallis Zn-Pb district in the Canadian Arctic archipelago contains numerous carbonatehosted mineralised showings, including the past-producing Polaris Zn-Pb mine on Little \nCornwallis Island. The showings’ mineralogy is primarily Zn-Pb, with anomalous Cu showings. \nThe volume and geographic/stratigraphic positions of mineralisation are variable, with the \nmajority being hosted by Middle Ordovician Thumb Mountain Formation limestone/dolostone \nadjacent to extensional faults. Multiple in situ micro-analytical techniques were used on samples \nfrom throughout the district to determine the origin, character, flow path, and age of the \nmineralizing fluid(s) responsible for the showings in the district, and to re-evaluate models of the \nPolaris deposit. \nGeochemical (fluid inclusion microthermometry, trace and rare earth elements, oxygen isotopes) \nresults indicate that a single, regional fluid was involved in mineralisation at all of the showings. \nSulphur isotopes indicate that pre-mineralisation sulphur accumulations at individual showings \naffected early mineralisation δ34S values until thermochemical sulphate reduction (TSR) of the \nregional fluid became the dominant sulphur supply, and that varying degrees of TSR completion \nresulted in showing-specific δ34S values, rather than a uniform regional value. The main control \non the volume of mineralisation was the amount of fluid flux that could be accommodated by the \nshowing, with Polaris being much larger than the rest because of its tectonic location, which \nallowed for copious amounts of mineralising fluid to interact with host rocks. The Storm copper showing on Somerset Island indicates that Cu showings in the Zn-Pb district \nare related to the regional fluids of the Zn-Pb showings, but local strata affected the mineralogy. \nThe geochemical signatures of the paragenetic stages indicate that pre-ore fluids were related to \nthe regional Zn-Pb fluid, whereas the main-ore fluid is related to a fluid that displaced the \nregional Zn-Pb-mineralising fluid during ongoing orogenesis. An underlying Proterozoic redbed \ncontains a record of diagenetic sequences and fluids that is similar to those responsible for the \nStorm copper showing, indicating that the geographically limited redbed was probably \nresponsible for the anomalous Cu-rich showing in the district.

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 score0.018
Threshold uncertainty score0.131

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.002
Science and technology studies0.0050.001
Scholarly communication0.0010.000
Open science0.0010.001
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0030.000

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 head0.008
GPT teacher head0.169
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 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
Published2020
Admission routes2
Has abstractyes

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