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Record W2538340214 · doi:10.3749/canmin.1500047

Mineral Chemistry of (Pt,Pd)-Bismuthotelluride Minerals In the Platreef At Zwartfontein, Akanani Project, Northern Bushveld Complex, South Africa

2015· article· en· W2538340214 on OpenAlexvenueno aff
Fanus Viljoen, Ntshebo Ramakoloi, Derek H. Rose, Christian Reinke

Bibliographic record

VenueThe Canadian Mineralogist · 2015
Typearticle
Languageen
FieldComputer Science
TopicGeochemistry and Geologic Mapping
Canadian institutionsnot available
FundersDepartment of Science and Technology, Ministry of Science and Technology, IndiaDSI-NRF Centre of Excellence for Integrated Mineral and Energy Resource AnalysisUniversity of JohannesburgNational Research FoundationNational Research Centre
KeywordsMineralGeologyGeochemistryMineralogyMining engineeringMetallurgyMaterials science

Abstract

fetched live from OpenAlex

The (Pt,Pd)-bismuthotelluride minerals at the Akanani prospect show substantial substitution of Te and Bi. Individual grains are often markedly heterogeneous with concentrations of Te and Bi which vary by up to 26 wt.%. They occur as single phase crystals or form composite grains with other platinum-group minerals, and are predominantly associated with ( i.e. , are in direct contact with) primary and secondary silicate minerals, base-metal sulfides, and magnetite. The Pt-bismuthotelluride minerals are markedly associated with ( i.e. , tends to occur as composite grains with) Pd-bismuthotelluride minerals, isoferroplatinum, and sperrylite. The Pd-bismuthotelluride minerals are markedly associated with Pt-bismuthotelluride minerals, altaite, hollingworthite, plumbopalladinite, PdSbSn alloy, and sperrylite. The Pt-bismuthotelluride minerals are characterized by high ratios of Te/Bi and form a trend of solid solution from moncheite (PtTe2) towards maslovite (PtTeBi). A few analyses plot close to, or on, the composition of maslovite. The Pd-bismuthotelluride minerals are characterized by a lower ratio of Te/Bi than the Pt-bismuthotelluride minerals. They form a trend of solid solution along the join kotulskite (PdTe)–sobolevskite (PdBi), without merenskyite (PdTe2). There is very limited solid solution of Pt and Pd between the Pt-bismuthotelluride minerals (<5.7 wt.% Pd) and the Pd-bismuthotelluride minerals (<3.3 wt.% Pt), with only four analyses of michenerite (three grains) characterized by elevated levels of Pd (10.3 to 17.1 wt.%). In view of the strong spatial association between the Pt- and Pd-bismuthotelluride minerals at Akanani it is considered likely that the latter were originally in solid solution in a precursor Pd-rich Pt-bismuthotelluride host at temperatures of up to 1150 °C, from which they then exsolved during cooling. Further exsolution of Te- or Bi-rich domains in individual Pt- and Pd-bismuthotelluride crystals occurred during late cooling at substantially lower temperatures, and resulted in the observed compositional ranges of moncheite–maslovite and kotulskite–sobolevskite.

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: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.066
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
Bibliometrics0.0020.001
Science and technology studies0.0010.000
Scholarly communication0.0010.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0020.000

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 head0.069
GPT teacher head0.237
Teacher spread0.167 · 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".

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Citations1
Published2015
Admission routes1
Has abstractyes

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