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Record W1766515772 · doi:10.3749/canmin.1400080

CHUBAROVITE, KZn<sub>2</sub>(BO<sub>3</sub>)Cl<sub>2</sub>, A NEW MINERAL SPECIES FROM THE TOLBACHIK VOLCANO, KAMCHATKA, RUSSIA

2015· article· en· W1766515772 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.
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 · 2015
Typearticle
Languageen
FieldMaterials Science
TopicCrystal Structures and Properties
Canadian institutionsnot available
Fundersnot available
KeywordsCrystallographyScoriaChemistryOrthoclaseMohs scale of mineral hardnessMineralMineralogyHaliteMuscoviteMicaGeologyGeochemistryVolcanoVolcanic rock

Abstract

fetched live from OpenAlex

The new mineral chubarovite, KZn 2 (BO 3 )Cl 2 , was found in the sublimates of active fumaroles at the Second and First scoria cones of the Northern Breakthrough of the Great Tolbachik Fissure Eruption, Tolbachik volcano, Kamchatka, Russia. At the Second scoria cone it occurs in the Arsenatnaya fumarole (the holotype) with fluoborite, krasheninnikovite, sylvite, halite, langbeinite, aphthitalite, orthoclase, fluorophlogopite, hematite, and tenorite. At the First scoria cone, chubarovite is closely associated with sellaite, fluorite, anhydrite, halite, cotunnite, challacolloite, sofiite, and flinteite. Chubarovite forms hexagonal or trigonal lamellar to tabular crystals up to 1.5 mm across and up to 0.5 mm thick, with aggregates and crystal crusts up to 1 cm across. The major crystal form is {001}, and lateral faces are {101}, {102}, {103}, {100}, and {110}; twins of two types are observed. Chubarovite is transparent, colorless, with vitreous luster. It is flexible but not elastic. The Mohs hardness is ca . 2. Cleavage is (001) perfect, mica-like. D (meas.) is 2.68(2), D (calc.) is 2.716 g cm –3 . Chubarovite is optically uniaxial (–), with ω 1.541(2), e 1.539(2). The infrared spectrum is given. Chemical data (wt.%, determined by electron-microprobe, boron by ICP OES) are: K 2 O 16.48, Rb 2 O 0.46, ZnO 53.96, B 2 O 3 10.98, Cl 24.48, –O=Cl 2 –5.53, total 100.83. The empirical formula, based on 5 (O+Cl) apfu , is: (K 1.05 Rb 0.01 ) Σ 1.06 Zn 2.00 B 0.95 O 2.92 Cl 2.08 . Chubarovite is trigonal, R 32, a 4.9429(4), c 26.348(2) A, V 557.50(8) A 3 , and Z = 3. The strongest reflections of the powder X-ray diffraction pattern [ d ,A( I )( hkl )] are: 8.79(100)(003), 4.394(43)(006), 4.225(25)(101), 4.074(91)(012), 3.590(90)(104), 3.324(30)(015), 2.470(67)(110), and 2.245(25)(1.0.10). Chubarovite has a novel structure type. Its crystal structure, solved from single-crystal X-ray diffraction data ( R = 0.020), is composed of layers of two types with an alternation along [001]. The anionic {Zn 2 (BO 3 )Cl 2 } – layer consists of flat triangular BO 3 groups sharing all O vertices with bases of ZnO 3 Cl tetrahedra. Each Cl atom is shared between one Zn-centered tetrahedron and three edge-connected KCl 6 octahedra belonging to the cationic layer formed by K + cations. The mineral is named in honor of the Russian mineralogist and physicist Valeriy M. Chubarov (born 1948).

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), Science and technology studies, Scholarly communication
Consensus categoriesnone
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 score0.511
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.001
Meta-epidemiology (narrow)0.0010.001
Meta-epidemiology (broad)0.0010.000
Bibliometrics0.0000.001
Science and technology studies0.0010.001
Scholarly communication0.0010.001
Open science0.0020.000
Research integrity0.0000.001
Insufficient payload (model declined to judge)0.0000.001

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 head0.030
GPT teacher head0.209
Teacher spread0.179 · 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