MétaCan
Menu
Back to cohort
Record W1983113771 · doi:10.2113/gscanmin.44.3.599

THE TANCO PEGMATITE AT BERNIC LAKE, MANITOBA. XVI. ZONAL AND BULK COMPOSITIONS AND THEIR PETROGENETIC SIGNIFICANCE

2006· article· en· W1983113771 on OpenAlexaffvenueabout
Andrew Stilling, P. Černý, P. J. Vanstone

Bibliographic record

VenueThe Canadian Mineralogist · 2006
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsUniversity of Manitoba
Fundersnot available
KeywordsPegmatiteGeologyGeochemistryPetrologyMineralogy

Abstract

fetched live from OpenAlex

The Tanco pegmatite deposit at Bernic Lake, in southeastern Manitoba, is a virtually completely hidden, essentially undeformed, subhorizontal, bilobate, saddle-shaped body ~1520 m long, 1060 m wide and up to ~100 m thick. The highly fractionated pegmatite of the LCT family, rare-element class, petalite subtype, consists of nine internal zones. The outer zones are concentric, whereas the layered inner zones are segmented and locally complex in shape. A 3D computer model representation of the pegmatite assisted in calculation of volumes and compositions of individual zones and of the whole pegmatite, based on 102 km of 1355 drill-hole intersections, underground observations, measured and estimated mineral modes of the zones, zone-specific compositions and densities of minerals, and ore grades. The early outer zones tend to show granitic modes, but the inner zones strongly deviate in proportions of feldspars, or by high enrichment in lithium minerals, and some of the zones are virtually monomineralic. The bulk mode of Tanco is granitic, except ~9 vol.% petalite (including spodumene + quartz pseudomorphs). Despite also being economically significant for Cs, Ta and Li, the pegmatite contains less than 1 vol.% of any other non-micaceous minerals, and less than 0.1% of most of them. The bulk chemical composition closely reflects the modal relationships: it is peraluminous, and granitic, with prominent enrichment in Li, Rb, Cs and F, moderate contents of Tl, Be, B, Ga, Sn, Nb and Ta, and remarkable depletion in Fe, Mn, Mg, Ca, Ba, Sc, Ti and Zr. A very high degree of fractionation is shown for the bulk pegmatite by the values K/Rb 4.7, K/Cs 9.3, Rb/Cs 2.0, Rb/Tl 137, Fe/Mn 0.63, Mg/Li 0.02, Al/Ga 917, Zr/Hf 2.6, Zr/Sn 0.21 and Nb/Ta 0.19. Zonal and bulk chemical composition is in rough agreement with the experimental thermal trough in the system Ab + Qtz + Ecr at 2 kbar P(H2O), but shifted toward the Ab apex by elevated B, P and F, and by the voluminous wall-zone. The composition of the wall zone (20) is remarkably similar to that of bulk Tanco, except for the elevated contents of rare elements in the latter that are concentrated in the intermediate and inner zones. In turn, zone (20) is very close to the composition of nearby, somewhat less fractionated peraluminous leucogranites that are parental to local genetically related pegmatite groups. The wall zone (20), which composes 44 vol.% of Tanco, represents by analogy a petrogenetic link between an undisclosed parent leucogranite and the Tanco deposit. These relationships document derivation of the Tanco pegmatite and its analogues elsewhere by igneous differentiation from a fertile leucogranitic magma.

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 machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.204
Threshold uncertainty score0.410

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.002
Science and technology studies0.0010.001
Scholarly communication0.0010.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0030.000

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 head0.008
GPT teacher head0.157
Teacher spread0.150 · 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 source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
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

Citations157
Published2006
Admission routes3
Has abstractyes

Explore more

Same venueThe Canadian MineralogistSame topicGeological and Geochemical AnalysisFrench-language works237,207