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Record W2148887584 · doi:10.2113/gscanmin.44.1.105

JOHNSENITE-(Ce): A NEW MEMBER OF THE EUDIALYTE GROUP FROM MONT SAINT-HILAIRE, QUEBEC, CANADA

2006· article· en· W2148887584 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.

affAt least one author lists a Canadian institution in the pinned OpenAlex snapshot.
venuePublished in a venue whose home country is Canada.
aboutThe title or abstract carries a Canadian signal from the geographic lexicon.

Bibliographic record

VenueThe Canadian Mineralogist · 2006
Typearticle
Languageen
FieldMaterials Science
TopicCrystal Structures and Properties
Canadian institutionsCanadian Museum of Nature
Fundersnot available
KeywordsSAINTGroup (periodic table)ChemistryComputer scienceComputer network

Abstract

fetched live from OpenAlex

La johnsenite-(Ce), de composition ideale Na 12 (Ce,La,Sr,Ca,□) 3 Ca 6 Mn 3 Zr 3 W (Si 25 O 73 ) (CO 3 )(OH,Cl) 2 , est un nouveau membre du groupe de l'eudyalite, decouvert au mont Saint-Hilaire, Quebec; il s'agit de l'analogue tungstenifere de la zirsilite-(Ce). Elle se presente en cristaux squelettiques fortement corrodes atteignant 4 mm, et 1 cm en aggregats. Lui sont associes albite, calcite, pectolite, aegyrine, fluorapophyllite, zirsilite-(Ce), un mineral du groupe de la burbankite, dawsonite, rhodochrosite, epididymite, galene, molybdenite, pyrite, pyrrhotite, quartz, une amphibole, sphalerite, stillwellite-(Ce), titanite, cerite-(Ce), tuperssuatsiaite, steacyite, catapleiite, zakharovite, natrolite et microcline. Elle est transparente a translucide, avec un eclat vitreux et une rayure blanche. Elle est cassante, avec une durete de Mohs de 5 a 6. Il n'y a aucun clivage ou plan de separation visible, et la fracture est inegale. Le mineral est uniaxe negatif, avec ω 1.648(1) et e 1.637(1). Sa symetrie est trigonale, groupe d'espace R3m, a 14.237(3) et c 30.03(1) A, V 5271(2) A 3 , Z = 3. Les huit raies les plus intenses du spectre de diffraction X (methode des poudres) [d en A (I)(hkl)] sont: 11,308(95)(101), 9.460(81)(012), 4.295(34)(205), 3.547(36)(220), 3.395(38)(131), 3.167(75)(217), 2.968(100)(315) et 2.849(81)(404). Nous presentons le spectre infrarouge de la johnsenite-(Ce). Les resultats de huit analyses a la microsonde electronique, dont trois sur le cristal ayant servi a l'ebauche de la structure, ont donne, en moyenne, Na 2 O 10.47, K 2 O 0.25, CaO 8.98, SrO 1.60 MnO 5.43, FeO 1.61, Y 2 O 3 0.70, La 2 O 3 1.56, Ce 2 O 3 3.01, Pr 2 O 3 1.14, Nd 2 O 3 0.89. Sm 2 O 3 0.12, Gd 2 O 3 0.33, Dy 2 O 3 0.14. TiO 2 0.73, ZrO 2 9.60, HfO 2 0.04, Nb 2 O 5 0.82, WO 3 5.23, SiO 2 43.16, Cl 0.77, CO 2 (1.27), H 2 O (0.32), O = Cl -0.17, pour un total de 97.99% (poids). La concentration de CO 2 et celle de H 2 O ont ete calculees selon la stoechiometrie etablie a partir de l'analyse de la structure. La formule empirique de la johnsenite-(Ce), fondee sur 29 atomes de (Si 4+ , Zr 4+ , Ti 4+ , Hf 4+ , Nb 5+ , W 6+ ) et un groupe (CO 3 ), selon les resultats de l'analyse structurale, est: Na 11.74 ([Ce 0.64 La 0.33 Dy 0.03 ]Σ 1.00 Sr 0.54 Ca 0.51 Y 0.22 K 0.19 ) Σ2.46 (Ca 5.06 [Pr 0.24 Nd 0.18 Gd 0.06 Sm 0.02 ]Σ 0.50 Mn 0.44 )Σ 0 (Mn 2.22 Fe 0.78 ) Σ3 (Zr 2.71 Ti 0.32 Hf 0.01 ) Σ3.04 (W 0.78 Nb 0.21 ) Σ0.99 Si 24.97 O 73 (CO 3 ) (OH,Cl 0.75 ) Σ2 , D meas . = 3.24(3) g/cm 3 ; D calc . = 3.23 g/cm 3 . La structure est faite de quatre couches, qui definissent une polarite, telle qu'indiquee par une analyse statistique des intensites des pics de diffraction, la composition des couches et le potentiel electrostatique des monocristaux. Le nom du mineral honore Ole Johnsen, du Musee Geologique, Universite de Copenhague, au Danemark.

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 score0.208
Threshold uncertainty score1.000

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 studies0.0000.000
Scholarly communication0.0000.000
Open science0.0010.000
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 head0.010
GPT teacher head0.177
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