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Record W6990628831

The effect of Li on the petrogenesis of granitic pegmatites

2015· dissertation· en· W6990628831 on OpenAlexfundaboutno aff

Bibliographic record

VenueeScholarship@McGill (McGill) · 2015
Typedissertation
Languageen
FieldEngineering
TopicScheduling and Optimization Algorithms
Canadian institutionsnot available
FundersNatural Sciences and Engineering Research Council of Canada
KeywordsPegmatitePetrogenesisCrystallizationSpodumeneAlbiteQuartzFeldsparSaturation (graph theory)Plagioclase
DOInot available

Abstract

fetched live from OpenAlex

The effect of Li on the petrogenesis of Li-bearing pegmatites was studied through a combination of experimental research and field investigations. Crystallization experiments were conducted under H2O-saturated and H2O-undersaturated conditions at 400-800 °C and 500 MPa, using a common granitic starting material (Li-free) and the same granitic material enriched with ~3700 ppm Li (Li-bearing). Comparison of the two sets of experiments highlighted the role of Li as an effective fluxing component of the pegmatite-forming melt; the presence of Li decreased the melting and crystallization temperatures, constrained the degree of undercooling at the onset of formation of pegmatitic textures to 85-110 °C, and increased the growth rates of feldspar crystals to 13 cm/y, one order of magnitude faster than feldspars grown in the Li-free system. Graphic and granophyric quartz-feldspar intergrowths, the characteristic textures encountered in pegmatites, were reproduced early in the Li-bearing experiments, followed by the development of K-feldspar, albite and quartz monomineralic zones at later stages, and the crystallization of Li-aluminosilicates close to the solidus.The experiments showed that Li preferentially partitioned in the melt, reaching ~12000 ppm at 80% crystallization. A new series of dissolution, crystallization and melting experiments at 550-750 °C and 500 MPa estimated the solubility of Li at the saturation of spodumene and petalite and defined the maximum saturation curve for Li-aluminosilicates. The results of these experiments suggested extreme Li enrichment of the pegmatite-forming melt before the formation of Li-aluminosilicate phases, often to the point of supersaturation (~22000 ppm Li at 600 °C). A comparison between the experimental results and information obtained from natural samples from the Moblan pegmatite in Quebec supported the extreme enrichment of the pegmatite-forming melt in Li, strengthening the plausibility of the supersaturation hypothesis. Lastly, based on the experimental results and the field observations on the Moblan pegmatite, the Li concentration of feldspar crystals was proposed as a useful exploration tool for the distinction between Li-free and Li-bearing pegmatites as well as the identification of Li-rich sections in an individual pegmatitic body. The geochemical signature of Li in feldspar, and possibly quartz as well, shows a promising potential as an inexpensive means to optimize targeting of Li-rich ore resources in pegmatites.

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)0.001
metaresearch head score (Gemma)0.002
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesMeta-epidemiology (narrow)
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 score0.913
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.002
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0010.000
Bibliometrics0.0000.001
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0010.000
Research integrity0.0000.001
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 head0.010
GPT teacher head0.222
Teacher spread0.212 · 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 designBench or experimental
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
Published2015
Admission routes2
Has abstractyes

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