MétaCan
Menu
Back to cohort
Record W1650417121

Deformation of Polymineralic Rocks by Replacement Creep

2001· article· en· W1650417121 on OpenAlex

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

affAt least one author lists a Canadian institution in the pinned OpenAlex snapshot.

Bibliographic record

Venueeag · 2001
Typearticle
Languageen
FieldEngineering
TopicGeotechnical and Geomechanical Engineering
Canadian institutionsQueen's University
Fundersnot available
KeywordsAnhydriteCalciteGeologyCreepMineralogyBiotiteDiffusion creepDeformation (meteorology)GeochemistryMaterials scienceMetallurgyGypsumGrain boundaryQuartz
DOInot available

Abstract

fetched live from OpenAlex

of magnitude lower than that of pure calcite rock or and 152 cm ; hence the volume-change of reaction pure anhydrite rock. Systematic curvature of the 1 is -34% (The solute species and the H O calcite/anhydrite interfaces supports my postulation molecules enter or leave the system in accord with that the predominant mechanism of deformation is reaction progress, so they make no contribution to replacement creep, a microstructural process the volume-change). For a rock under tectonic governed by the rules of diffusion metasomatism. stress, this provides a thermodynamic prediction: In this case, replacement creep approximates to Albite will tend to replace biotite at interfaces constant-calcium replacement of anhydrite by calcite at interfaces normal to the maximum principal stress (σ ) and of calcite by anhydrite at 1 interfaces normal to the minimum principal stress (σ ). Fundamental to replacement creep is a 3

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.

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 categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Simulation or modeling · Consensus signal: Simulation or modeling
GenreCandidate signal: Empirical · Consensus signal: none
Teacher disagreement score0.727
Threshold uncertainty score0.259

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)0.0000.000

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 head0.004
GPT teacher head0.173
Teacher spread0.169 · 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