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Record W2583937309 · doi:10.3749/canmin.1500035

Compositional Variations of Apatite, Fractionation Trends, and A Pge-Bearing Zone In the Kivakka Layered Intrusion, Northern Karelia, Russia

2016· article· en· W2583937309 on OpenAlexvenueno aff
A.Yu. Barkov, Andrey A. Nikiforov

Bibliographic record

VenueThe Canadian Mineralogist · 2016
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsnot available
Fundersnot available
KeywordsLayered intrusionGeologyIntrusionGeochemistryApatiteFractionationBearing (navigation)MineralogyGeographyChemistryCartography

Abstract

fetched live from OpenAlex

Abstract The ∼3.5 km thick Kivakka complex (2.45 Ga) in northern Karelia hosts a zone of disseminated Pd-Pt-Ni-Cu mineralization near its base. The zone is related to a special or “critical horizon” and displays relative maxima in bulk-rock concentrations of Cu, Ni, Co, and Cr, in the ratios Cu:Ni, Cu:Zr, and 100Fe 2 O 3 /(FeO + Fe 2 O 3 ), and elevated levels of Cr in ortho- and clinopyroxene, along with higher levels of incompatible Ti, V, and Zr. Early crystallizing minerals (highly magnesian pyroxenes and An-rich plagioclase) are associated in this zone with 1–10% (commonly 3 to 5%) base-metal sulfides (BMS) and interstitial phases [nearly pure Ab, chlorapatite, zircon, Fe-(Ti) oxides, etc .]. Apatite is characterized by extensive variations in Cl (both intragranular and intergranular), which attain the composition of chlorapatite (>6 wt.% Cl), not observed below the zone. The compositional trend of the apatite series is extensive; the content of F generally increases upward, whereas Cl decreases, with the observed maximum (3.3% F) near the top of the intrusion. The PGE-rich zone is inferred to have formed at the “critical level” as a consequence of a combination of several factors. Factor 1 represents an abrupt change in the sequence and character of cumulus phases; a massive crystallization of cumulate An 75–81 is accompanied by a sharp decrease in the amount of orthopyroxene with cessation of crystallization of olivine. As a likely result, the remaining melt became substantially enriched in Cr. Alternatively, the Cr enrichment is related to an influx of a new portion of magma. Factor 2 represents a rise in levels of oxygen fugacity, f (O 2 ). Factor 3 is displayed by the sharp increase in Cl in the intercumulus apatite; the fractionated melt well above this zone appears to be depleted in Cl. The sudden drop in Cl is attributed to degassing of the melt, from which a Cl-rich volatile phase exsolved, causing fractionation of Cl from F. Factor 4 involves an increase in levels of sulfur fugacity, f (S 2 ), resulting in the deposition of the disseminated BMS in association with tiny grains of Pd-Pt bismuthotellurides and sperrylite. Thus, the formation of PGE mineralization appears to have proceeded in Kivakka as a sequence of processes and events, rather than as a result of a single factor or process during fractional crystallization of the complex.

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 score0.021
Threshold uncertainty score0.041

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.001
Science and technology studies0.0010.000
Scholarly communication0.0010.000
Open science0.0000.001
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 head0.192
Teacher spread0.180 · 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

Citations14
Published2016
Admission routes1
Has abstractyes

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