MétaCan
Menu
Back to cohort
Record W2942360997 · doi:10.21954/ou.ro.0000e7db

Geochronology and geochemistry of rare-element pegmatites from the Superior Province of Canada

2001· dissertation· en· W2942360997 on OpenAlexaboutno aff
S. R. Smith

Bibliographic record

VenueOpen Research Online (The Open University) · 2001
Typedissertation
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsnot available
Fundersnot available
KeywordsPegmatiteMuscoviteGeologyGeochemistryColumbiteSolidusAnatexisGeochronologyLithophilePartial meltingQuartzCrustPaleontologyMaterials sciencePhase (matter)Chemistry

Abstract

fetched live from OpenAlex

The crystallisation age and thermochronology of late- to post-orogenic, rare-lithophile element (Li, Cs, Ta) pegmatites that are chemically associated with peraluminous granites have been determined from U-Pb TIMS and LA-MC-ICP-MS analyses of columbite-tantalite, and UV -laser <sup>40</sup>Ar/<sup>39</sup>Ar analyses of mica. <br><br>In the northwest Superior Province, U-Pb ages reveal that the Pakeagama Lake pegmatite crystallised at 2673 ±8Ma. Rare-element pegmatites in the western Superior Province yield crystallisation ages of 2649 ±4Ma and 2644 ±8Ma for the Separation Rapids group, and 2665 ±lOMa for the Mavis Lake group, showing that they are temporally associated with adjacent peraluminous granites. Replacement zones of columbite-tantalite grains from the pegmatites show disturbance to the U-Pb system, probably caused by interaction with residual fluids and sub solidus metasomatic processes that lasted for -30Ma after crystallisation. <br><br>Mica from rare-element pegmatites is characterised by distinct compositional zoning with muscovite cores and F-, Li- and Rb-rich zinnwalditellepidolite rims. The zinnwalditellepidolite rims that replace the original muscovite were most likely precipitated from a residual melt or fluid phase during the late-magmatic to hydrothermal period of pegmatite formation. <br><br>Within these micas, <sup>40</sup>Ar/<sup>39</sup>Ar apparent ages young towards the grain boundary and also towards the core - rim boundary, which suggests that the compositional zones form separate argon diffusion domains. However, similar <sup>40</sup>Ar/<sup>39</sup>Ar apparent ages are found within F-rich zinnwaldite/lepidolite and coexisting muscovite indicating that diffusion rates may be comparable. <br><br>Mica from rare-element pegmatites of the Superior Province yield intra-grain <sup>40</sup>Ar/<sup>39</sup>Ar apparent age variations of up to 800Ma within single crystals. Theoretical slow cooling models do not match the measured <sup>40</sup>Ar/<sup>39</sup>Ar profiles and cannot account for the large apparent age variations. Thermal history models that produce the best fit to apparent age profiles include two re-heating events; a minimum 350°C re-heating at -2450Ma and <i>circa</i> 300°C re-heating at 1850Ma, both for a period of at least 10Ma. These apparent ages are concordant with two major Proterozoic events affecting the Superior Province; intrusion of the Matachewan - Hearst dyke swarms and the Trans Hudson Orogeny, respectively.

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 categoriesInsufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.242
Threshold uncertainty score0.985

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0030.001
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0160.000

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 head0.033
GPT teacher head0.272
Teacher spread0.240 · 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 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
Published2001
Admission routes1
Has abstractyes

Explore more

Same venueOpen Research Online (The Open University)Same topicGeological and Geochemical AnalysisFrench-language works237,207