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Record W2155661238 · doi:10.1180/minmag.2009.073.3.487

Fluoro-sodic-ferropedrizite, NaLi<sub>2</sub>(Fe<sub>2</sub><sup>2+</sup>Al<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 Sutlug River, Tuva Republic, Russia: description and crystal structure

2009· article· en· W2155661238 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 · 2009
Typearticle
Languageen
FieldMaterials Science
TopicCrystal Structures and Properties
Canadian institutionsUniversity of Manitoba
Fundersnot available
KeywordsMohs scale of mineral hardnessCrystallographyPegmatiteAcicularMonoclinic crystal systemPleochroismMineralogyAmphiboleCleavage (geology)Materials scienceCrystal structureChemistryQuartzGeologyFracture (geology)MetallurgyMicrostructureComposite material

Abstract

fetched live from OpenAlex

Abstract Fluoro-sodic-ferropedrizite, ideally A Na B Li 2 C ( ) T Si 8 O 22 W F2, is a new mineral of the amphibole group from the Sutlug River, Tuva Republic, Russia. It occurs at the endogenic contact of a Li-pegmatite with country rocks near to a diabase dyke and formed by reaction of the pegmatitic melt with the country rock. Fluoro-sodic-ferropedrizite occurs as prismatic to acicular crystals, ranging in length from 0.1–3 cm and widths of up to 50 μm. Crystals occur inparallel to sub-parallel aggregates up to 5 mm across ina matrix of calcite and plagioclase feldspar. Crystals are pale bluish-grey with a greyish-white streak. Fluoro-sodic-ferropedrizite 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 3.116 g cm –3 . In plane-polarized light, it is pleochroic, X = pale purple-grey, Y = light grey, Z = colourless; X ^ a = 71.2º (in β acute), Y || b , Z ^ c = 83.4º (in β obtuse). Fluoro-sodic-ferropedrizite is biaxial positive, α = 1.642(1), β = 1.644(1), γ = 1.652(1); 2V (obs) = 68.0(3)º, 2V (calc) = 56.4º. Fluoro-sodic-ferropedrizite is monoclinic, space group C 2/ m, a = 9.3720(4) Å, b = 17.6312(8) Å, c = 5.2732(3) Å, β = 102.247(4)º, V = 851.5(2) Å 3 , Z = 2. The strongest ten X-ray diffraction lines in the powder patternare ( d in Å ,( I ),( hkl )): 8.146,(10),(110); 2.686,(9),(151); 3.008,(8),(310); 4.430,(7),(021); 2.485,(6),( 02); 3.383,(4),(131); 2.876,(3),( 51, 11); 2.199,(3),( 12); 4.030,(2),(111) and 3.795,(2),( 31). Analysis by a combination of electron microprobe and crystal-structure refinement gives SiO 2 59.81, Al 2 O 3 12.66, TiO 2 0.09, FeO 10.32, MgO 5.56, MnO 0.73, ZnO 0.17, CaO 0.20, Na 2 O 2.81, Li 2 O 4.80, F 2.43, H 2 O calc 1.10, sum = 99.65 wt.%. The formula unit, calculated on the basis of 24(O,OH,F) is A (Na 0.68 ) B (Li 1.92 Na 0.05 Ca 0.03 ) C ( ) T (Si 7.98 Al 0.02 )O 22 W (F 1.03 OH 0.97 ). Crystal-structure refinement shows Li to be completely ordered at the M(3) and M(4) sites. Fluoro-sodic-ferropedrizite, ideally A Na B Li 2 C ( ) T Si 8 O 22 W F2, is related to the theoretical end-member ‘sodic-pedrizite’, A Na B Li 2 C (Mg 2 Al 2 Li) T Si 8 O 22 W (OH) 2 , by the substitutions C Fe 2+ → C Mg and W F → W (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)0.002
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 score0.108
Threshold uncertainty score0.999

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0020.002
Meta-epidemiology (narrow)0.0040.003
Meta-epidemiology (broad)0.0040.002
Bibliometrics0.0010.003
Science and technology studies0.0020.003
Scholarly communication0.0020.003
Open science0.0040.003
Research integrity0.0020.003
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 head0.013
GPT teacher head0.204
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