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Record W7029696545

Linking deformation and diffusion to develop a strain speedometer

2015· dissertation· en· W7029696545 on OpenAlexfundno aff

Bibliographic record

VenueeScholarship@McGill (McGill) · 2015
Typedissertation
Languageen
FieldArts and Humanities
TopicLibraries and Information Services
Canadian institutionsnot available
FundersFonds de recherche du Québec – Nature et technologiesNatural Sciences and Engineering Research Council of CanadaMcGill University
KeywordsDeformation (meteorology)DiffusionPlagioclaseStrain rateStrain (injury)Atomic diffusionCompression (physics)Diffusion process
DOInot available

Abstract

fetched live from OpenAlex

I present the first comprehensive study of strain-enhanced diffusion in plagioclase through a multiscale, theoretical and physical approach. First I argue from first principles that diffusion and deformation are both processes of breaking and reforming bonds that take energy in order to proceed. Deformation can enhance diffusion by supplying strain energy that facilitates breaking bonds and by mobilizing dislocations, which can act as pathways for atomic migration. Widely-used geologic tools such as geochronometers and geothermobarometers neglect deformation-enhanced diffusion, which may lower closure temperatures and reset ages, temperatures, and pressures, leading to erroneous values calculated based on static diffusion or no diffusion after conditions of interest. If deformation enhancement of element mobility is measurable, we may be able to calculate and account for the effects of deformation on these calculations. The connection between deformation and diffusion also provides an opportunity to link deformation with a time-dependent process and infer strain rate. Strain rate is an integral parameter in understanding crustal deformation and cannot be directly determined from the rock record in most cases. To evaluate strain enhanced diffusion in a common rock forming mineral, I combined field-scale, thin-section scale, and grain-scale strain and chemical measurements for major and trace elements in naturally deformed plagioclase phenocrysts from the San José Pluton, Peninsular Ranges Batholith, México. The multiscale approach made it possible to connect grain-scale strain with bulk-rock deformation through methods I developed. I used high spatial resolution, sensitive, in situ analyses using electron probe micro-analysis (EPMA) and Laser Ablation Inductively Coupled Plasma Mass Spectrometry (LA-ICP-MS) to correlate changes in shape (strain) and chemical composition (element mobility). I conclude that at low strain and low compositional contrast between primary growth zones measured, the effect of strain-enhanced element mobility, as predicted from my model, is too subtle to quantify using available analytical techniques. This means that for such a set of conditions, a static diffusion model is sufficient, and geothermobarometers and geochronometers can still be applied to yield accurate results. Future work should explore the relationships between different variables affecting strain enhanced element mobility, such as thermal history, strain, strain rate, and starting compositions, to refine the applicability of existing tools and the potential for new ones.

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)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesMeta-epidemiology (narrow), Science and technology studies, Insufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Not applicable · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.951
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
Meta-epidemiology (narrow)0.0010.001
Meta-epidemiology (broad)0.0010.000
Bibliometrics0.0010.000
Science and technology studies0.0010.000
Scholarly communication0.0010.004
Open science0.0000.000
Research integrity0.0000.001
Insufficient payload (model declined to judge)0.0010.001

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 head0.032
GPT teacher head0.235
Teacher spread0.203 · 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 designNot applicable
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 routes1
Has abstractyes

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