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Record W2170678805 · doi:10.1093/petrology/egq074

Global Variability in the Platinum-group Element Contents of Komatiites

2010· article· en· W2170678805 on OpenAlexaff
Marco L. Fiorentini, Stephen J. Barnes, Wolfgang D. Maier, O Marcus Burnham, G. J. Heggie

Bibliographic record

VenueJournal of Petrology · 2010
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsGeological Survey of Canada
Fundersnot available
KeywordsGreenstone beltArcheanGeologyGeochemistryPlatinum groupTerraneCratonMantle (geology)Mantle plumeOlivinePlatinumTectonicsPaleontologyChemistryLithosphere

Abstract

fetched live from OpenAlex

Platinum-group element (PGE) concentrations in komatiites of similar age but different petrological affinity, lithofacies type and emplacement style are remarkably similar when the effects of olivine fractionation and accumulation are accounted for. All komatiites display a slight enrichment of PPGE (Rh, Pt and Pd) over IPGE (Ir, Ru and Os) attributable to limited retention of IPGE in their mantle sources, coupled with saturation in Ir–(Os) alloys. Significant differences and trends exist, however, including subtle provinciality in Pt/Pd ratios, and in particular a systematic linear increase in komatiite PGE contents with age from the oldest at >3·5 Ga to the late Archaean group at c. 2·7 Ga, regardless of petrogenetic type. There is a linear secular trend of increasing Pt at a given MgO content and in Pt/Ti from 3500 Ma to 2700 Ma across all komatiite types. Barberton-type komatiites younger than 3000 Ma are generally slightly depleted in Pt and Pd relative to Munro-type. Munro-type komatiites from 3200–3500 Ga greenstone belts of the east Pilbara Craton of Western Australia are strongly depleted in PGE relative to younger belts, but similar to Barberton-type komatiites of the same age. Munro-type and Barberton-type komatiites from the 2900 Ma greenstone belts of the Youanmi Terrane in the Yilgarn Craton have similar PGE contents. Age, rather than komatiite type, appears to be the dominant control. These observations lead us to the hypothesis that the age control is related to a secular variation in the PGE content of komatiite mantle source regions. We envisage that Early Archaean komatiites could have been derived from plumes sourced in the deep mantle, which had been largely stripped of its highly siderophile element budget during core segregation and as yet incompletely replenished in PGE by the Late Veneer. Late Archaean komatiites have higher PGE contents as a result of progressive mixing-in of Late Veneer material over the period between the Late Heavy Bombardment (4·3–3·9 Ga) and 2·7 Ga, at which time the mantle had become effectively homogeneous with respect to PGE. The relative constancy of gamma-osmium values in komatiites throughout the Archaean is consistent with this hypothesis.

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 score0.004
Threshold uncertainty score0.009

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.001
Science and technology studies0.0000.000
Scholarly communication0.0000.000
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 head0.009
GPT teacher head0.214
Teacher spread0.205 · 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

Citations85
Published2010
Admission routes1
Has abstractyes

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