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Record W2101799757 · doi:10.1180/minmag.2013.077.6.09

The dumortierite supergroup. I. A new nomenclature for the dumortierite and holtite groups

2013· article· en· W2101799757 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 · 2013
Typearticle
Languageen
FieldMaterials Science
TopicCrystal Structures and Properties
Canadian institutionsUniversity of British Columbia
Fundersnot available
KeywordsSupergroupIsostructuralNomenclatureGroup (periodic table)OctahedronCrystallographyChemistryMineralStereochemistryCrystal structureGeologyGeochemistryBiology

Abstract

fetched live from OpenAlex

Abstract Although the distinction between magnesiodumortieite and dumortierite, i.e. Mg vs . Al dominance at the partially vacant octahedral Al1 site, had met current criteria of the IMA Commission on New Minerals, Nomenclature and Classification (CNMNC) for distinguishing mineral species, the distinction between holtite and dumortierite had not, since Al and Si are dominant over Ta and (Sb, As) at the Al1 and two Si sites, respectively, in both minerals. Recent studies have revealed extensive solid solution between Al, Ti, Ta and Nb at Al1 and between Si, As and Sb at the two Si sites or nearly coincident (As, Sb) sites in dumortierite and holtite, further blurring the distinction between the two minerals. This situation necessitated revision in the nomenclature of the dumortierite group. The newly constituted dumortierite supergroup, space group Pnma (no. 62), comprises two groups and six minerals, one of which is the first member of a potential third group, all isostructural with dumortierite. The supergroup, which has been approved by the CNMNC, is based on more specific end-member compositions for dumortierite and holtite, in which occupancy of the Al1 site is critical. (1) Dumortierite group, with Al1 = Al 3+ , Mg 2+ and ☐, where ☐ denotes cation vacancy. Charge balance is provided by OH substitution for O at the O 2 , O 7 and O10 sites. In addition to dumortierite, endmember composition AlAl 6 BSi 3 O 18 , and magnesiodumortierite, endmember composition MgAl 6 BSi 3 O 17 (OH), plus three endmembers, “hydroxydumortierite”, ☐Al 6 BSi 3 O 15 (OH) 3 and two Mg-Ti analogues of dumortierite, (Mg 0.5 Ti 0.5 )Al 6 BSi 3 O 18 and (Mg 0.5 Ti 0.5 )Mg 2 Al 4 BSi 3 O 16 (OH) 2 , none of which correspond to mineral species. Three more hypothetical endmembers are derived by homovalent substitutions of Fe 3+ for Al and Fe 2+ for Mg. (2) Holtite group, with Al1 = Ta 5+ , Nb 5+ , Ti 4+ and ☐. In contrast to the dumortierite group, vacancies serve not only to balance the extra charge introduced by the incorporation of pentavalent and quadrivalent cations for trivalent cations at Al1, but also to reduce repulsion between the highly charged cations. This group includes holtite, endmember composition (Ta 0.6 ☐ 0.4 )Al 6 BSi 3 O 18 , nioboholite (2012-68), endmember composition (Nb 0.6 ☐ 0.4 )Al 6 BSi 3 O 18 , and titanoholtite (2012-69), endmember composition (Ti 0.75 ☐ 0.25 )Al 6 BSi 3 O 18 . (3) Szklaryite (2012-70) with Al1 = ☐ and an endmember formula ☐Al 6 BAs 3+ 3 O 15 . Vacancies at Al1 are caused by loss of O at O 2 and O 7 , which coordinate the Al1 with the Si sites, due to replacement of Si 4+ by As 3+ and Sb 3+ , and thus this mineral does not belong in either the dumortierite or the holtite group. Although szklaryite is distinguished by the mechanism introducing vacancies at the Al1 site, the primary criterion for identifying it is based on occupancy of the Si/As, Sb sites: (As 3+ + Sb 3+ ) > Si 4+ consistent with the dominant-valency rule. A Sb 3+ analogue to szklaryite is possible.

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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)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesInsufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Bench or experimental · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.917
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0010.000
Scholarly communication0.0010.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

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 head0.212
Teacher spread0.200 · 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