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Record W7162011478 · doi:10.82308/4996

Illitization and chloritization of illitesmectite and chloritesmectite mixed-layer clays in high-grade diagenetic and very low-grade metamorphic environments of Gaspe Peninsula, Quebec Appalachians, Canada : problems and solutions

2000· dissertation· en· W7162011478 on OpenAlexaboutno aff
Salah. Shata

Bibliographic record

Venuenot available
Typedissertation
Languageen
FieldMaterials Science
TopicClay minerals and soil interactions
Canadian institutionsnot available
Fundersnot available
KeywordsDiagenesisChloriteIlliteMetamorphic rockSedimentary rockMineral

Abstract

fetched live from OpenAlex

The present study deals with three main mineralogical and geochemical problems related to the behaviour of two common clay minerals---illite and chlorite---in the Lower Paleozoic sedimentary sequences of high-grade diagenetic and very low grade metamorphic (VLGM) zones in the Quebec Appalachians, Gaspe Peninsula. In high-grade diagenetic to VLGM zones, illite and chlorite coexist, but as they are notoriously fine-grained and intimately intergrown, tracing the chemical changes in chlorite with conventional (wet chemical method or electron microprobe) methods is a difficult task. A refined XRD method for the determination of the structural formula of chlorites was developed in this study. Application of this program to high-grade diagenetic to VLGM chlorite from the Gaspe Peninsula revealed that these chlorites are of "ripidolitic" to "pycnochloritic" composition and show a compositional homogenization in the anchizone, as compared to chlorite of the diagenetic zone. With increasing metamorphic grade, chlorites become less siliceous, have decreasing octahedral-site vacancies, and approach the ideal trioctahedral chlorite composition. Although Fe-asymmetry increases, the [Fe (total)] decreases, which may reflect a preferential decrease in [Fe (total)] in the brucite-like sheet. At high (>80%) illite levels in mixed-layer illite smectite, the gradual improvement of illite crystallinity (IC), coupled with advancing VLGM conditions, suggests some modification of the clay mineral structure, possibly involving loss of the still existing expandable layers. Failure to detect expandable components in anchimetamorphic illitic materials upon glycolation has led previous investigators to rule out the existence of expandable components beyond the high-grade diagenetic zone. X-ray diffraction (XRD) patterns and high-resolution transmission electron images of n-alkylammonium-cation-treated clay minerals showed the presence of expandable layers in high-grade diagenetic to VLGM phyllosilicates and document the impact of these expandable layers on IC measurements. With advancing diagenetic to VLGM grade, the intermediate metastable phases of a rectorite-like R1-ordered layer structure, either with an intermediate or high-charge vermiculite interface, and an R3-ordered structure are found in the fine fraction. (Abstract shortened by UMI.)

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 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 score0.868
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0010.000
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)0.0000.000

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 head0.011
GPT teacher head0.209
Teacher spread0.198 · 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
Published2000
Admission routes1
Has abstractyes

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