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Record W1947585262 · doi:10.3749/canmin.48.1.95

LECOQITE-(Y), Na3Y(CO3)3{middle dot}6H2O, A NEW MINERAL SPECIES FROM MONT SAINT-HILAIRE, QUEBEC, CANADA

2010· article· en· W1947585262 on OpenAlex

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

venuePublished in a venue whose home country is Canada.
aboutThe title or abstract carries a Canadian signal from the geographic lexicon.
no affNo Canadian affiliation: this work is invisible to an affiliation-only frame.
No Canadian affiliation. An affiliation-only frame, the usual design, would never have seen this work. It is one of the works that make the case for inverting the frame.

Bibliographic record

VenueThe Canadian Mineralogist · 2010
Typearticle
Languageen
FieldMaterials Science
TopicCrystal Structures and Properties
Canadian institutionsnot available
Fundersnot available
KeywordsSAINTMineralGeologyGeochemistryGeographyMaterials scienceArtMetallurgyArt history

Abstract

fetched live from OpenAlex

Lecoqite-(Y), ideally Na 3 Y(CO 3 ) 3 ·6H 2 O, a new mineral species, was discovered at the Poudrette quarry, Mont Saint-Hilaire, Quebec, Canada. It is associated with microcline, albite, natrolite, gonnardite, aegirine, siderite, elpidite, gaidonnayite, zircon, franconite, dawsonite, rhodochrosite, cryolite, rutile, and sphalerite. Lecoqite-(Y) forms radiating, spray-like aggregates in compact, tightly packed masses to 2.5 cm across, composed of flexible, extremely thin, capillary crystals up to 2.5 cm long and up to 0.01 mm thick. Individuals are colorless, and aggregates are white. The luster is strikingly silky. D(calc.) = 2.358 g/cm 3 . Lecoqite-(Y) is optically uniaxial positive, ω = 1.521(3), e = 1.497(3). The IR spectrum is unique. The chemical composition (electron microprobe, H 2 O by modified Penfield method, CO 2 by selective absorption, average results) is: Na 2 O 19.22, CaO 0.03, Y 2 O 3 17.95, Nd 2 O 3 0.54, Sm 2 O 3 0.41, Gd 2 O 3 0.75, Dy 2 O 3 3.31, Ho 2 O 3 1.12, Er 2 O 3 3.20, Yb 2 O 3 1.48, CO 2 27.0, H 2 O 23.4, total 98.41 wt.%. The empirical formula calculated for 15 O apfu is: Na 2.94 (Y 0.755 Dy 0.085 Er 0.08 Yb 0.035 Ho 0.03 Gd 0.02 Nd 0.015 Sm 0.01 ) ∑1.03 (CO 3 ) 2.91 (OH) 0.21 (H 2 O) 6.06 . Lecoqite-(Y) is hexagonal, P 6 3 , a 11.316(4), c 5.931(2) A, V 657.7(4) A 3 , Z = 2. The crystal structure was established from X-ray powder data by the Rietveld method, based on the model of the isostructural synthetic Ln-free carbonate Na 3 Y(CO 3 ) 3 ·6H 2 O. Final agreement factors are: R p = 0.0468, R wp = 0.0657, R Bragg = 0.0343, R F = 0.0356. No mineral is closely related to lecoqite-(Y) in terms of structure. In the structure of lecoqite-(Y), REE atoms (REE = Y + Ln) are surrounded by six O atoms of CO 3 groups and three H 2 O molecules to form a tricapped triangular prism. The Na atoms are centered in distorted octahedra [NaO 4 (H 2 O) 2 ], which link to form infinite corrugated chains along c . The strongest five lines of the X-ray powder pattern [ d in A (I)( hkl )] are: 9.82(57)(100), 5.081(100)(101), 3.779(39)(201), 2.627(39)(112), 2.471(37)(131). Lecoqite-(Y) is named in memory of P.E. Lecoq de Boisbaudran (1838–1912), outstanding French chemist and specialist in the spectroscopic analysis of minerals and synthetic compounds, who made a great contribution to the chemistry of the rare-earth elements. The Levinson suffix modifier -(Y) is in line with the dominance of yttrium over other rare-earth elements in the mineral. The cotype specimens are deposited in the Fersman Mineralogical Museum of Russian Academy of Sciences, Moscow, and the Canadian Museum of Nature, Ottawa.

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.

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: Not applicable · Consensus signal: Not applicable
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.415
Threshold uncertainty score0.994

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 studies0.0010.000
Scholarly communication0.0010.000
Open science0.0010.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0070.000

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 head0.018
GPT teacher head0.185
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