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Record W2337749884 · doi:10.2138/am-2016-5359

Maruyamaite, K(MgAl <sub>2</sub> )(Al <sub>5</sub> Mg)Si <sub>6</sub> O <sub>18</sub> (BO <sub>3</sub> ) <sub>3</sub> (OH) <sub>3</sub> O, a potassium-dominant tourmaline from the ultrahigh-pressure Kokchetav massif, northern Kazakhstan: Description and crystal structure

2016· article· en· W2337749884 on OpenAlexaff
Aaron J. Lussier, Neil A. Ball, F. C. Hawthorne, Darrell J. Henry, R. Shimizu, Yoshihide Ogasawara, Tsutomu Ota

Bibliographic record

VenueAmerican Mineralogist · 2016
Typearticle
Languageen
FieldMaterials Science
TopicCrystal Structures and Properties
Canadian institutionsUniversity of Manitoba
Fundersnot available
KeywordsPleochroismCrystallographyMohs scale of mineral hardnessCrystal structureMineralogyMineralCorundumChemistryMaterials scienceMetallurgy

Abstract

fetched live from OpenAlex

Maruyamaite, ideally K(MgAl 2 )(Al 5 Mg)Si 6 O 18 (BO 3 ) 3 (OH) 3 O, was recently approved as the first K-dominant mineral-species of the tourmaline supergroup. It occurs in ultrahigh-pressure quartzofeldspathic gneisses of the Kumdy-Kol area of the Kokchetav Massif, northern Kazakhstan. Maruyamaite contains inclusions of microdiamonds, and probably crystallized near the peak pressure conditions of UHP metamorphism in the stability field of diamond. Crystals occur as anhedral to euhedral grains up to 2 mm across, embedded in a matrix of anhedral quartz and K-feldspar. Maruyamaite is pale brown to brown with a white to very pale-brown streak and has a vitreous luster. It is brittle and has a Mohs hardness of ∼7; it is non-fluorescent, has no observable cleavage or parting, and has a calculated density of 3.081 g/cm 3 . In plane-polarized transmitted light, it is pleochroic, O = darkish brown, E = pale brown. Maruyamaite is uniaxial negative, ω = 1.634, ε = 1.652, both ±0.002. It is rhombohedral, space group R3m , a = 15.955(1), c = 7.227(1) Å, V = 1593(3) Å 3 , Z = 3. The strongest 10 X-ray dif- fraction lines in the powder pattern are [ d in Å( I )( hkl )]: 2.581(100)(051), 2.974(85)(1̄32), 3.995 (69)(2̄40), 4.237(59)(2̄31), 2.046(54)(1̄62), 3.498(42)(012), 1.923(36)(3̄72), 6.415(23)(1̄11), 1.595(22)(5̄.10.0), 5.002(21)(021), and 4.610(20)(030). The crystal structure of maruyamaite was refined to an R 1 index of 1.58% using 1149 unique reflections measured with Mo K α X-radiation. Analysis by a combination of electron microprobe and crystal-structure refinement gave SiO 2 36.37, Al 2 O 3 31.50, TiO 2 1.09, Cr 2 O 3 0.04, Fe 2 O 3 0.33, FeO 4.01, MgO 9.00, CaO 1.47, Na 2 O 0.60, K 2 O 2.54, F 0.30, B 2 O 3 (calc) 10.58, H 2 O(calc) 2.96, sum 100.67 wt%. The formula unit, calculated on the basis of 31 anions pfu with B = 3, OH = 3.24 apfu (derived from the crystal structure) and the site populations assigned to reflect the mean interatomic distances, is (K 0.53 Na 0.19 Ca 0.26 □ 0.02 ) ΣX=1.00 (Mg 1.19 Fe0.552+Fe0.053+${\rm{Fe}}_{0.55}^{2 + }{\rm{Fe}}_{0.05}^{3 + }$ Ti 0.14 Al 1.07 ) □Y=3.00 (Al 5.00 Mg 1.00 )(Si 5.97 Al 0.03 O 18 )(BO 3 ) 3 (OH) 3 (O0.602−${\rm{O}}_{0.60}^{2 - }$F 0.16 OH 0.24 ). Maruyamaite, ideally K(MgAl 2 ) (Al 5 Mg)(BO 3 ) 3 (Si 6 O 18 )(OH) 3 O, is related to oxy-dravite: ideally Na(MgAl 2 )(Al 5 Mg)(BO 3 ) 3 (Si 6 O 18 )(OH) 3 O, by the substitution X K → X Na.

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: Bench or experimental · Consensus signal: Bench or experimental
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.007
Threshold uncertainty score0.017

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.001
Science and technology studies0.0010.000
Scholarly communication0.0010.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0050.002

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 head0.011
GPT teacher head0.207
Teacher spread0.196 · 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 designBench or experimental
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".

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Citations34
Published2016
Admission routes1
Has abstractyes

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