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Record W2110381872 · doi:10.2113/gscanmin.42.5.1357

EXPERIMENTAL SIMULATION OF SHOCK-INDUCED RE-EQUILIBRATION OF FLUID INCLUSIONS

2004· article· en· W2110381872 on OpenAlexvenueno aff
M. E. Elwood Madden, F. Hörz, Robert J. Bodnar

Bibliographic record

VenueThe Canadian Mineralogist · 2004
Typearticle
Languageen
FieldPhysics and Astronomy
TopicAstro and Planetary Science
Canadian institutionsnot available
Fundersnot available
KeywordsShock (circulatory)GeologyFluid inclusionsMechanicsPhysicsSeismologyMedicine

Abstract

fetched live from OpenAlex

Les impacts meteoritiques et les ondes de choc qui en resultent creent des conditions favorisant des taux de deformation, des temperatures et des pressions extremement eleves. A mesure que le role des phases fluides dans notre systeme solaire attire de plus en plus d'attention, il est essentiel de bien comprendre les effets des ondes de choc sur les materiaux a composantes fluides. Ce travail porte sur les effects d'une onde de choc d'entre 5 et 30 GPa generee experimentalement sur les inclusions fluides aqueuses piegees dans des monocristaux de quartz. La temperature d'homogeneisation de ces inclusions et d'autres caracteristiques physiques ont ete documentees avant et apres l'evenement de choc. Les proprietes des inclusions fluides montrent une evolution graduelle et systematique a mesure qu'augmente l'intensite de l'onde de choc. Certaines inclusions survivent a une pression de choc de 6 GPa, mais elles montrent une augmentation de la temperature d'homogeneisation par rapport aux inclusions avant l'impact, ce qui indique un re-equilibrage a cause d'une surpression interne. Nous avons remarque des inclusions fluides decrepitees a 6 et a 7.6 GPa, tandis que les textures indicatives d'un affaissement des inclusions fluides a cause du developpement d'un vide de decompression ont ete observees dans les echantillons dont l'onde de choc faisait entre 7.6 et 12 GPa. Nous ne voyons aucun signe de la presence d'inclusions fluides dans les echantillons sujets a une pression transitoire depassant 12 GPa. Les resultats de ces experiences font penser que les inclusions fluides subissent d'abord une diminution en volume due a la decompression transitoire. Si elles survivent a ce stade, cette diminution initiale est renversee a cause des effets d'une temperature elevee a pression ambiante, ce qui mene a une augmentation du volume et de la temperature d'homogeneisation. C'est donc dire que la temperature d'homogeneisation des inclusions fluides dans les materiaux ayant subi un metamorphisme de choc aurait une valeur maximale, parce que la densite de la phase fluide piegee a l'origine etait-probablement superieure a celle qui est observee dans les inclusions ayant subi un choc. D'apres ces resultats, il semble que la rarete des inclusions fluides dans les meteorites pourrait resulter d'un remaniage du au choc, et non de l'absence relative de fluides dans le milieu de formation de la meteorite.

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)0.001
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Simulation or modeling · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.005
Threshold uncertainty score0.015

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
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 science0.0010.000
Research integrity0.0010.001
Insufficient payload (model declined to judge)0.0040.000

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 head0.024
GPT teacher head0.260
Teacher spread0.236 · 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 designSimulation or modeling
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

Citations6
Published2004
Admission routes1
Has abstractyes

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