MétaCan
Menu
Back to cohort
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 OpenAlexaffvenueabout
J. D. Grice, R. A. Gault

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.

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 score0.064
Threshold uncertainty score0.128

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.002
Science and technology studies0.0040.001
Scholarly communication0.0010.000
Open science0.0010.001
Research integrity0.0010.000
Insufficient payload (model declined to judge)0.0070.001

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

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

Citations24
Published2006
Admission routes3
Has abstractyes

Explore more

Same venueThe Canadian MineralogistSame topicCrystal Structures and PropertiesFrench-language works237,207