MétaCan
Menu
Back to cohort
Record W4382050646 · doi:10.3749/2200052

Characterizing Zinc-Rich Chromite Cores and Uvarovite-Grossular Garnet Mantles from the Pikoo Property, Central Eastern Saskatchewan, Canada

2023· article· en· W4382050646 on OpenAlexaffabout
Song Gao, Kerri Campbell, R. L. Flemming, Ken Armstrong, B. Kupsch

Bibliographic record

VenueThe Canadian Journal of Mineralogy and Petrology · 2023
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsWestern University
Fundersnot available
KeywordsChromiteGeologyMetasomatismGrossularZincGeochemistryMineralogyAndraditePetrographyMaterials scienceMetallurgyFluid inclusionsSkarnHydrothermal circulation

Abstract

fetched live from OpenAlex

Abstract Zinc-rich chromite, (Fe,Zn)Cr2O4, is an important repository for chromium (Cr) that has been observed sporadically worldwide. As another source for Cr, green uvarovite garnet, ideally Ca3Cr2(SiO4)3, is the rarest variety among anhydrous garnets. Here, we present a detailed petrographic, mineralogical, and geochemical characterization of 71 uvarovite garnets with zinc-bearing chromite cores recovered from the Pikoo Property (central eastern Saskatchewan), which also hosts recently discovered kimberlites proven to be diamondiferous. In this work, euhedral to anhedral unzoned chromite occurs as cores or irregular inclusions enclosed by uvarovite–grossular mantles. They contain moderate to high Cr (41.63–66.70 wt.% Cr2O3; Cr/(Cr+Al) = 0.64–0.99), Fe2+ (16.71–28.67 wt.% FeO), and Zn (1.64–15.52 wt.% ZnO) contents, accompanied by an appreciable amount of Mn (0.63–2.32 wt.% MnO). The chromite core with the highest Zn content gave the structural formula (Zn0.409Fe2+0.555Mg0.018Mn0.019)Σ1.00(Cr1.174Al0.674Fe3+0.152)Σ2.00O4, which corresponds to Zn-rich chromite with a minor proportion of other endmembers (e.g., hercynite, FeAl2O4). Zinc enrichment in chromite is most likely the result of metasomatic replacement of primary chromite involving the action of Zn-rich fluids. The Zn-rich chromite cores are commonly porous and demonstrate streaking in the 2D diffraction pattern that is attributable to non-uniform strain. The strain measurements suggest the involvement of fluid-present plastic deformation during metasomatic alteration. The garnets are compositionally zoned aggregates and commonly contain inclusions. Chemical formulae indicate that they are mainly members of the uvarovite–grossular series (up to 93% mol.% Uv) enriched in Ca (22.99–35.57 wt.% CaO) and Cr (up to 28.10 wt.% Cr2O3), but consistently depleted in Mg (mean = 0.10 wt.% MgO) and Ti (mean = 0.26 wt.% TiO2). Most garnet aggregates consist of uvarovite and grossular that exhibit a core-rim zoning pattern characterized by an increase in grossular proportion at the expense of the uvarovite component. Morphological characteristics, textural relations, and compositional trends suggest that uvarovite garnet formed through interaction of Zn-rich chromite with grossular. This mineral assemblage is not genetically related to the Pikoo kimberlite and represents an independent evolutionary event. The use of Zn-bearing chromite as a new kimberlite indicator mineral therefore should be carefully evaluated prior to exploration practices.

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 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 score0.050
Threshold uncertainty score1.000

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)0.0010.000

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 head0.012
GPT teacher head0.168
Teacher spread0.156 · 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
Published2023
Admission routes2
Has abstractyes

Explore more

Same venueThe Canadian Journal of Mineralogy and PetrologySame topicGeological and Geochemical AnalysisFrench-language works237,207