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Record W2600129693 · doi:10.1180/minmag.2016.080.103

Fogoite-(Y), Na<sub>3</sub>Ca<sub>2</sub>Y<sub>2</sub>Ti(Si<sub>2</sub>O<sub>7</sub>)<sub>2</sub>OF<sub>3</sub>, a Group I TS-block mineral from the Lagoa do Fogo, the Fogo volcano, São Miguel Island, the Azores: Description and crystal structure

2017· article· en· W2600129693 on OpenAlexafffund
Fernando Cámara, Elena Sokolova, Y. A. Abdu, F. C. Hawthorne, T. Charrier, Vincent Dorcet, Jean‐François Carpentier

Bibliographic record

VenueMineralogical Magazine · 2017
Typearticle
Languageen
FieldMaterials Science
TopicCrystal Structures and Properties
Canadian institutionsUniversity of Manitoba
FundersNatural Sciences and Engineering Research Council of CanadaU.S. Geological SurveyUniversità degli Studi di Torino
KeywordsTriclinic crystal systemMohs scale of mineral hardnessCrystallographyElectron microprobeQuartzMineralogyMaterials scienceAnalytical Chemistry (journal)Crystal structureChemistryMetallurgy

Abstract

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Abstract Fogoite-(Y), Na3Ca2Y2Ti(Si2O7)2OF3, is a new mineral from the Lagoa do Fogo, São Miguel Island, the Azores. It occurs in cavities as highly elongated (on [001]) prisms, up to 2000 μm long and 50 μm× 50 μm in cross-section, associated with sanidine, astrophyllite, fluornatropyrochlore, ferrokentbrooksite, quartz and ferro-katophorite. Crystals are generally transparent and colourless, with vitreous lustre, occasionally creamy white. Fogoite-(Y) has a white streak, splintery fracture and very good {100} cleavage. Mohs hardness is ∼5.Dcalc.= 3.523 g/cm3. It is biaxial (+) with refractive indices (λ = 590 nm) α = 1.686(2), β = 1.690(2), γ = 1.702(5); 2Vmeas.= 57(1)° and 2Vcalc.= 60°. It is nonpleochroic. Fogoite-(Y) is triclinic, space groupP1,a= 9.575(6),b= 5.685(4),c= 7.279(5) Å, α = 89.985(6), β = 100.933(4), γ = 101.300(5)°,V= 381.2 (7) Å3. The six strongest reflections in the powder X-ray diffraction data [d(Å), I, (hkl)] are: 2.954, 100, (1̄1̄2, 3̄10); 3.069, 42, (300, 01̄2); 2.486, 24, (310, 21̄2); 3.960, 23, (1̄1̄1, 2̄10); 2.626, 21, (2̄20); 1.820, 20, (1̄04). Electron microprobe analysis gave the following empirical formula calculated on 18 (O + F) (Na2.74Mn0.15)∑2.89Ca2[Y1.21(La0.01Ce0.03Nd0.03Sm0.02Gd0.08Dy0.08Er0.05Yb0.04Lu0.01)∑0.35Mn0.16Zr0.11Na0.09Fe0.072+Ca0.01]∑2(Ti0.76Nb0.23Ta0.01)∑1(Si4.03O14)O1.12F2.88,Z= 1. The crystal structure was refined on a twinnedcrystal toR1= 2.81% on the basis of 2157 unique reflections (Fo> 4σFo) and is a framework of TS (Titanium Silicate) blocks, which consist of HOH sheets (H – heteropolyhedral, O – octahedral) parallel to (100). In the O sheet, the the[6]MO(1) site is occupied mainly by Ti, O(1)–ϕ> = 1.980 Å, and the[6]MO(2) and[6]MO(3) sites are occupied by Na and Na plus minor Mn, O(2)–ϕ>= 2.490 Å and O(3)–ϕ> = 2.378 Å. In the H sheet, the two[4]Si sites are occupied by Si, with = 1.623 Å; the[6]MHsite is occupied by Y and rare-earth elements (Y >REE), with minor Mn, Zr, Na, Fe2+and Ca, H–ϕ> = 2.271 Å and the[6]APsite is occupied by Ca, <AP–ϕ> = 2.416 Å. The MHand APoctahedra and Si2O7groups constitute the H sheet. The ideal compositions of the O and two H sheets are Na3Ti(OF)F2and Y2Ca2(Si2O7)2apfu. Fogoite-(Y) is isostructural with götzenite and hainite. The mineral is named after the type locality, the Fogo volcano in the Azores.

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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: Bench or experimental · Consensus signal: Bench or experimental
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.036
Threshold uncertainty score0.071

Distilled classifier scores by category (both heads)

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 head0.015
GPT teacher head0.215
Teacher spread0.200 · 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 designBench or experimental
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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Citations9
Published2017
Admission routes2
Has abstractyes

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