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Record W2327461881 · doi:10.1180/minmag.2012.076.5.05

Ianbruceite, ideally [Zn<sub>2</sub>(OH)(H<sub>2</sub>O)(AsO<sub>4</sub>)](H<sub>2</sub>O)<sub>2</sub>, a new arsenate mineral from the Tsumeb mine, Otjikoto (Oshikoto) region, Namibia: description and crystal structure

2012· article· en· W2327461881 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.

fundA Canadian funder is recorded on the work.
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

VenueMineralogical Magazine · 2012
Typearticle
Languageen
FieldMaterials Science
TopicCrystal Structures and Properties
Canadian institutionsnot available
FundersNatural Sciences and Engineering Research Council of CanadaCanada Research Chairs
KeywordsCrystallographyMohs scale of mineral hardnessElectron microprobeMonoclinic crystal systemPleochroismChemistryMineralogyPlatyAnalytical Chemistry (journal)OctahedronCrystal structureMaterials science

Abstract

fetched live from OpenAlex

Abstract Ianbruceite, ideally [Zn 2 (OH)(H 2 O)(AsO 4 )](H 2 O) 2 , is a new supergene mineral from the Tsumeb mine, Otjikoto (Oshikoto) region, Namibia. It occurs as thin platy crystals up to 80 μm long and a few μm thick, which form flattened aggregates up to 0.10 mm across, and ellipsoidal aggregates up to 0.5 mm across. It is associated with coarse white leiteite, dark blue köttigite, minor legrandite and adamite. Ianbruceite is sky blue to very pale blue with a white streak and a vitreous lustre; it does not fluoresce under ultraviolet light. It has perfect cleavage parallel to (100), is flexible, and deforms plastically. The Mohs hardness is 1 and the calculated density is 3.197 g cm -3 . The refractive indices are α = 1.601, β = 1.660, γ = 1.662, all ±0.002; 2V obs = 18(2)°, 2V calc = 20°, and the dispersion is r &lt; v , weak. Ianbruceite is monoclinic, space group P 2 1 / c, a = 11.793(2), b = 9.1138(14), c = 6.8265(10) Å, β = 103.859(9)°, V = 712.3(3) Å 3 , Z = 4, a:b:c = 1.2940:1:0.7490. The seven strongest lines in the X-ray powder diffraction pattern [ d (Å), I , ( hkl )] are as follows: 11.29, 100, (100); 2.922, 17, (130); 3.143, 15, (202); 3.744, 11, (300); 2.655, 9, (230); 1.598, 8, (152); 2.252, 7, (222). Chemical analysis by electron microprobe gave As 2 O 5 36.27, As 2 O 3 1.26, Al 2 O 3 0.37, ZnO 49.72, MnO 0.32, FeO 0.71, K 2 O 0.25, H 2 O calc 19.89, sum 108.79 wt.%; the very high oxide sum is due to the fact that the calculated H 2 O content is determined from crystal-structure analysis, but H 2 O is lost under vacuum in the electron microprobe. The crystal structure of ianbruceite was solved by direct methods and refined to an R 1 index of 8.6%. The As is tetrahedrally coordinated by four O anions with a mean As O distance of 1.687 Å. Zigzag [ [5] Zn [6] Znϕ 7 ] chains extend in the c direction and are linked in the b direction by sharing corners with (AsO 4 ) tetrahedra to form slabs with a composition [Zn 2 (OH)(H 2 O)(AsO 4 )]. The space between these slabs is filled with disordered (H 2 O) groups and minor lone-pair stereoactive As 3+ . The ideal formula derived from chemical analysis and crystal-structure solution and refinement is [Zn 2 (OH)(H 2 O)(AsO 4 )](H 2 O) 2 .

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), 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 score0.123
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0020.001
Meta-epidemiology (narrow)0.0040.003
Meta-epidemiology (broad)0.0030.001
Bibliometrics0.0010.002
Science and technology studies0.0020.002
Scholarly communication0.0020.003
Open science0.0020.002
Research integrity0.0020.003
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 head0.019
GPT teacher head0.212
Teacher spread0.193 · 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