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Record W2594221836 · doi:10.1180/minmag.2016.080.088

Lobanovite, K<sub>2</sub>Na(Fe<sub>4</sub><sup>2+</sup>Mg<sub>2</sub>Na)Ti<sub>2</sub>(Si<sub>4</sub>O<sub>12</sub>)<sub>2</sub>O<sub>2</sub>(OH)<sub>4</sub>, a new mineral of the astrophyllite supergroup and its relation to magnesioastrophyllite

2017· article· en· W2594221836 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 · 2017
Typearticle
Languageen
FieldMaterials Science
TopicCrystal Structures and Properties
Canadian institutionsUniversity of Manitoba
Fundersnot available
KeywordsMonoclinic crystal systemCrystallographyKola peninsulaPegmatiteMineralogyMassifStructural formulaMineralChemistryCrystal structureGeologyMaterials scienceGeochemistryMetallurgy

Abstract

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Abstract Lobanovite, K 2 Na(Fe 4 2+ Mg 2 Na)Ti 2 (Si 4 O 12 ) 2 O 2 (OH) 4 , is a new mineral of the astrophyllite supergroup from Mt. Yukspor, the Khibiny alkaline massif, Kola Peninsula Russia. It has been known previously under the following names: monoclinic astrophyllite, magnesium astrophyllite, magnesiumastrophyllite and magnesioastrophyllite but has never been formally proposed and approved as a valid mineral species by the Commission on new Minerals, Nomenclature and Classification of the International Mineralogical Association. It has now been revalidated and named lobanovite after Dr. Konstantin V. Lobanov, a prominent Russian ore geologist who worked in the Kola Peninsula for more than forty years (Nomenclature voting proposal 15-B). Lobanovite has been described from pegmatitic cavities on Mt. Yukspor where it occurs as elongated bladed crystals, up to 0.04 mm wide and 0.2 mm long, with a straw yellow to orange colour. Associated minerals are shcherbakovite, lamprophyllite, delindeite, wadeite, umbite and kostylevite. Lobanovite is biaxial (–) with refractive indices (λ = 589 nm) α = 1.658, β calc . = 1.687, γ = 1.710; 2V meas. = 81.5– 83°. Lobanovite is monoclinic, space group C 2/ m , a = 5.3327(2), b = 23.1535(9), c = 10.3775(4) Å, β = 99.615(1)°, V = 1263.3 (1) Å 3 , Z = 2. The six strongest reflections in the powder X-ray diffraction data [ d (Å), I, ( hkl )] are: 3.38, 100, (003); 2.548, 90, (063); 10.1, 80, (001); 3.80, 60, (042,131); 3.079, 50, (132,062); 2.763, 90, (1̄71). The chemical composition of lobanovite was determined by electron-microprobe analysis and the empirical formula (K 1.97 Ba 0.01 ) ∑1.98 (Na 0.65 Ca 0.14 ) ∑0.79 (Fe 3.18 2+ Mg 2.02 Na 1.00 Mn 0.72 ) ∑6.92 (Ti 1.99 Nb 0.06 ) ∑2.05 [(Si 8.01 Al 0.06 ) ∑8.07 O 24 ]O 2 (OH) 4.03 F 0.19 was calculated on the basis of 30.2 (O + OH + F) anions, with H 2 O calculated from structure refinement, D calc. = 3.161 g cm –3 . In the structure of lobanovite, the main structural unit is the HOH block, which consists of one close-packed O (Octahedral) and two H (Heteropolyhedral) sheets. The M(1–4) octahedra form the O sheet and the T 4 O 12 astrophyllite ribbons and [5]-coordinated Ti-dominant D polyhedra link through common vertices to form the H sheet. The HOH blocks repeat along [001], and K and Na atoms occur at the interstitial A and B sites. The simplified and end-member formulae of lobanovite are K 2 Na [(Fe 2+ ,Mn) 4 Mg 2 Na]Ti 2 (Si 4 O 12 ) 2 O 2 (OH) 4 and K 2 Na(Fe 4 2+ Mg 2 Na)Ti 2 (Si 4 O 12 ) 2 O 2 (OH) 4 , respectively.

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)0.006
metaresearch head score (Gemma)0.005
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesMeta-epidemiology (narrow), Science and technology studies, Scholarly communication, Open science, Research integrity, Insufficient payload (model declined to judge)
Consensus categoriesMeta-epidemiology (narrow), Science and technology studies, Open science, Research integrity
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 score0.068
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0060.005
Meta-epidemiology (narrow)0.0110.009
Meta-epidemiology (broad)0.0100.005
Bibliometrics0.0030.006
Science and technology studies0.0060.006
Scholarly communication0.0060.007
Open science0.0090.008
Research integrity0.0060.008
Insufficient payload (model declined to judge)0.0000.004

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 head0.016
GPT teacher head0.218
Teacher spread0.203 · 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