MétaCan
Menu
Back to cohort
Record W4383370518 · doi:10.3749/2200026

Oscillatory Zoned Liddicoatite from Anjanabonoina, Central Madagascar. III. Trace Elements

2023· article· en· W4383370518 on OpenAlexaff
Aaron J. Lussier, F. C. Hawthorne

Bibliographic record

VenueThe Canadian Journal of Mineralogy and Petrology · 2023
Typearticle
Languageen
FieldMaterials Science
TopicCrystal Structures and Properties
Canadian institutionsUniversity of ManitobaCanadian Museum of Nature
Fundersnot available
KeywordsTrace elementGeologyAmplitudeCrystal (programming language)MineralogyOscillation (cell signaling)Analytical Chemistry (journal)ChemistryPhysicsGeochemistryOptics

Abstract

fetched live from OpenAlex

Abstract Large crystals of liddicoatite (tourmaline) from the Anjanabonoina Pegmatite of Central Madagascar are well-known for their distinct patterns of oscillatory zoning. This study follows two previous investigations, in which the crystal chemistry (Lussier et al. 2011a) and variations of major chemical constituents (Lussier & Hawthorne 2011) were characterized in detail. Here, the variations of elements present only at the trace level are investigated. The measurement by laser ablation inductively coupled plasma mass spectrometry of 26 trace elements, with abundances spanning four orders of magnitude (∼10−1 to 103 ppm) is reported. Trace elements were analyzed along continuous analytical traverses from the core to the rim of the crystal. Abundance profiles for most of the trace elements quantified (21 of 26) show clear oscillations that coincide with optical oscillatory zoning features. Throughout the crystal, the occurrence of compositional oscillation is independent of trace-element abundance; even where mean abundance is low, ∼1 ppm (e.g., V3+, Y3+, Th4+), oscillatory behavior is clear. Conversely, the magnitude of the oscillatory amplitude shows a strong near-linear dependence on element abundance. Within individual oscillatory zones, four unique line-shapes are observed, each differentiated by (1) the direction of a compositional discontinuity at the zone limits and (2) the orientation of the nonlinear curvature across the zone. For any individual zone, the variation in element concentration, C, can be fitted to the equation C = ±Aeλ(x−Φ)+ Δ where A is the zone amplitude; Φ is a reference position, and λi and Δi are fitted parameters. Comparison of the fitted equations shows that linear correlation between element pairs is common, occurring between pairs consisting of trace–trace, trace–major, and major–major elements. The oscillatory behavior of constituent elements is related to the location of the trace element in the tourmaline structure, with elements at the X- and Y-sites typically showing increases and decreases in abundance over single oscillatory zones. Throughout each zone, Mg has high abundance (∼104 ppm) at the start of each zone, followed by an extremely abrupt decrease in abundance, typically over a distance of <1 mm, making its behavior different to that of other elements (both trace and major). Finally, there are systematic differences in trace-element abundances between pyramid {201} and prism {100} sectors of the crystal, echoing the differences observed for major elements between these two sectors and consistent with face-dependent differences in element uptake.

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 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: Observational · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.588
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 studies0.0000.000
Scholarly communication0.0000.000
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 head0.209
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 teacher head, not a consensus.

Study designObservational
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".

Quick stats

Citations0
Published2023
Admission routes1
Has abstractyes

Explore more

Same venueThe Canadian Journal of Mineralogy and PetrologySame topicCrystal Structures and PropertiesFrench-language works237,207