MétaCan
Menu
Back to cohort
Record W2028028298 · doi:10.1180/minmag.2010.074.3.441

Noonkanbahite, BaKNaTi<sub>2</sub>(Si<sub>4</sub>O<sub>12</sub>)O<sub>2</sub>, a new mineral species: description and crystal structure

2010· article· en· W2028028298 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.

Bibliographic record

VenueMineralogical Magazine · 2010
Typearticle
Languageen
FieldMaterials Science
TopicCrystal Structures and Properties
Canadian institutionsLakehead UniversityUniversity of ManitobaQueen's University
Fundersnot available
KeywordsOrthorhombic crystal systemPleochroismCrystallographyCrystal structureMaterials scienceLamellar structureCleavage (geology)MineralogyChemistry

Abstract

fetched live from OpenAlex

Abstract Noonkanbahite, ideally BaKNaTi 2 (Si 4 O 12 )O 2 , is described as a new mineral species. At Liley [Löhley], Eifel Mountains, Germany (the holotype locality), it occurs as sprays of prismatic crystals (up to 8 mm) or single prismatic crystals (up to 4 mm) on walls of cavities in alkaline igneous rocks. At Murun, Siberia, Russia, noonkanbahite forms coarse lamellar crystals up to 0.05 cm × 0.7 cm × 1.5 cm embedded in kalsilite syenite. Noonkanbahite is brittle, H = 6, D obs. = 3.39(1), D calc. = 3.49 g/cm 3 , has a vitreous lustre and does not fluoresce in ultraviolet light. It has poor cleavage on {010} and {100} and weak parting on {011}. Noonkanbahite is biaxial positive with 2V obs. = 75(2)°, 2V calc. = 72.7(9)°, α 1.730(5), β 1.740(5) and γ 1.765(5), dispersion is medium, r &lt; v . In transmitted plane-polarized light, noonkanbahite is strongly pleochroic, with X colourless, Y yellowish, Z straw-yellow; X = a , Y = b , Z = c . Noonkanbahite is orthorhombic, space group Imma , a = 8.0884(4), b = 10.4970(5), c = 13.9372(6) Å, V = 1183.3(1) Å 3 , Z = 4. The strongest ten X-ray diffraction lines in the powder pattern [ d in Å ( I )( hkl )] are: 2.907(100)(222), 8.353(50)(001), 3.196(50)(220), 2.097(50)(242), 2.241(40)(215), 2.179(40)(035), 3.377(30)(031), 2.694(30)(015), 2.304(30)(233), and 1.564(30)(064). Electron microprobe analysis gives SiO 2 37.82, TiO 2 15.54, ZrO 2 0.42, Nb 2 O 5 3.18, Al 2 O 3 0.17, Fe 2 O 3 (recalculated from FeO) 5.63, MnO 0.32, MgO 0.53, BaO 20.60, CaO 1.36, K 2 O 5.32, Na 2 O 6.14, F 0.78, H 2 O 0.58, sum 98.39 wt.%, (H 2 O determined by SIMS). The formula unit, calculated on the basis of 14 anions (O+OH+F), is (Ba 0.85 K 0.13 ) Σ 0.98 (K 0.59 Na 0.26 Ca 0.15 ) Σ1.00 Na(Ti 1.23 Fe 0.45 3+ Nb 0.15 Mg 0.08 Mn 0.03 Zr 0.02 Al 0.01 ) Σ 1.97 (Si 3.99 Al 0.01 O 12 )(O 1.33 OH 0.41 F 0.26 ) Σ 2.00 , Z = 4. The crystal structure was refined to R 1 = 2.8% for 970 unique ( F 0 &gt; 4σ F ) reflections collected on a Bruker single-crystal P 4 diffractometer with a CCD detector and M o K α X-radiation. The crystal structure of noonkanbahite is isostructural with that of batisite, ideally BaNa 2 Ti 2 (Si 4 O 12 )O 2 , and scherbakovite, ideally K 2 NaTi 2 (Si 4 O 12 )O(OH). There are two octahedrally coordinated sites, M (1) and M (2), occupied by (Ti 1.23 Fe 0.45 3+ Nb 0.15 Mg 0.08 Mn 0.03 Zr 0.02 Al 0.01 ), ideally Ti 2 a.p.f.u. There are three interstitial A sites, [9] A (1), [8] A (2) and [6] A (3), occupied by Ba, K and Na, respectively. Si tetrahedra and M octahedra form a framework with interstitial cages occupied by Ba, K and Na atoms at the A sites. Noonkanbahite, BaKNaTi 2 (Si 4 O 12 )O 2 , is a K analogue of batisite, BaNa 2 Ti 2 (Si 4 O 12 )O 2 , and a Ba analogue of shcherbakovite, K 2 NaTi 2 (Si 4 O 12 )O(OH).

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)0.001
metaresearch head score (Gemma)0.001
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesMeta-epidemiology (narrow), Scholarly communication, Research integrity, Insufficient payload (model declined to judge)
Consensus categoriesMeta-epidemiology (narrow)
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 score0.065
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.001
Meta-epidemiology (narrow)0.0020.001
Meta-epidemiology (broad)0.0020.001
Bibliometrics0.0000.001
Science and technology studies0.0010.001
Scholarly communication0.0010.001
Open science0.0010.001
Research integrity0.0010.002
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 head0.206
Teacher spread0.191 · 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