MétaCan
Menu
Back to cohort
Record W2057193944 · doi:10.1180/minmag.2010.074.3.521

Fluoroleakeite, NaNa<sub>2</sub>(Mg<sub>2</sub>Fe<sup>3+</sup><sub>2</sub>Li)Si<sub>8</sub>O<sub>22</sub>F<sub>2</sub>, a new mineral of the amphibole group from the Verkhnee Espe deposit, Akjailyautas Mountains, Eastern Kazakhstan District, Kazakhstan: description and crystal structure

2010· article· en· W2057193944 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 institutionsUniversity of Manitoba
Fundersnot available
KeywordsPleochroismMohs scale of mineral hardnessCrystallographyMonoclinic crystal systemAmphiboleCleavage (geology)AegirineMineralogyActinolitePyriteBiotiteChemistryQuartzMineralCrystal structureEpidoteGeologyMaterials scienceChloriteFracture (geology)Metallurgy

Abstract

fetched live from OpenAlex

Abstract Fluoroleakeite, NaNa 2 (Mg 2 Fe 3+ 2 Li)Si 8 O 22 F 2 is a new mineral of the amphibole group from the Verkhnee Espe deposit, Akjailyautas mountains, eastern Kazakhstan district, Kazakhstan. The granites and their host rocks have been intensely reworked by post-magmatic and host-rock fluids, resulting in intense recrystallization, enrichment in F, Li and rare elements, and replacement of primary biotite and sodic-calcic amphiboles by Li-bearing riebeckite, aegirine, astrophyllite and other sodic minerals including fluoroleakeite. Crystals are prismatic parallel to [001] with {100} and {110} faces and cleavage surfaces, and the prism direction is terminated by irregular fractures. Grains are up to 3 mm long, and occur as isolated crystals, as small aggregates, and as inclusions in cámaraite. Crystals are black with a very pale grey to colourless streak. Fluoroleakeite is brittle, has a Mohs hardness of 6 and a splintery fracture; it is non-fluorescent with perfect {110} cleavage, no observable parting, and has a calculated density of 3.245 g cm –3 . In plane-polarized light, it is pleochroic, X = pale grey-green, Y = medium grey, Z = grey-brown; X ^ a = 14.1° (in β obtuse), Y ‖ b , Z ^ c = 75.9° (in β acute). Fluoroleakeite is biaxial negative, α = 1.663(2), β = 1.673(2), γ = 1.680(2); 2V obs = 80.9(6)°, 2V calc = 79.4° Fluoro-leakeite is monoclinic, space group C 2/ m , a = 9.8927(3), b = 17.9257(6), c = 5.2969(2) Å, β = 103.990(1)°, V = 905.7(1) Å 3 , Z = 2. The strongest ten X-ray diffraction lines in the powder pattern are [ d in Å( I )( hkl )]: 2.718(100)(151), 8.434(40)(110), 4.464(30)(021), 3.405(30)(131), 3.137(20)(310), 2.541(20)( ), 2.166(20)(261), 2.325(15)( ), 2.275(15)( ) and 2.806(10)(330). Analysis by a combination of electron microprobe and crystal-structure refinement gives SiO 2 53.34, Al 2 O 3 0.62, TiO 2 1.27, V 2 O 3 0.05, Fe 2 O 3 15.10, FeO 6.00, MnO 2.04, ZnO 0.18, MgO 6.40, CaO 0.13, Na 2 O 9.08, K 2 O 1.98, Li 2 O 1.10, F 3.33, H 2 O calc 0.16, sum 99.39 wt.%. The formula unit, calculated on the basis of 23 O, is A (Na 0.64 K 0.38 )(Na 1.98 Ca 0.02 )(Li 0.66 Mg 1.42 Fe 0.75 2+ Mn 0.26 2+ Zn 0.02 Fe 1.69 3+ V 0.01 3+ Ti 0.14 4+ Al 0.03 ) (Si 7.93 Al 0.07 )O 22 (F 1.57 OH 0.16 O 0.27 ). Crystal-structure refinement shows Li to be completely ordered at the M (3) site. Fluoroleakeite, ideally NaNa 2 (Mg 2 Fe 2 3+ Li)Si 8 O 22 F 2 , is related to end-member leakeite, NaNa 2 (Mg 2 Fe 2 3+ Li)Si 8 O 22 (OH) 2 by the substitution F → (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)0.002
metaresearch head score (Gemma)0.001
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesMeta-epidemiology (narrow), Science and technology studies, Scholarly communication, Research integrity
Consensus categoriesMeta-epidemiology (narrow), Science and technology studies, 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 score0.099
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0020.001
Meta-epidemiology (narrow)0.0040.003
Meta-epidemiology (broad)0.0040.002
Bibliometrics0.0010.003
Science and technology studies0.0020.003
Scholarly communication0.0030.002
Open science0.0040.003
Research integrity0.0030.004
Insufficient payload (model declined to judge)0.0000.000

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 head0.009
GPT teacher head0.192
Teacher spread0.183 · 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