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Record W2008557522 · doi:10.1139/t01-101

Application de la scanographie à l'étude de la densité des sédiments et à la caractérisation des structures sédimentaires : exemple des sédiments déposés dans la rivière Saguenay (Québec, Canada) après la crue de juillet 1996

2002· article· en· W2008557522 on OpenAlexvenueaboutno aff
Jean-François Crémer, Bernard Long, Gaston Desrosiers, Laure de Montety, Jacques Locat

Bibliographic record

VenueCanadian Geotechnical Journal · 2002
Typearticle
Languageen
FieldEnvironmental Science
TopicHydrology and Sediment Transport Processes
Canadian institutionsnot available
Fundersnot available
KeywordsGeologySedimentary rockGeomorphologySedimentVarveBioturbationDeposition (geology)TurbiditeTurbidity currentFjordGeochemistryStructural basinSedimentary depositional environment

Abstract

fetched live from OpenAlex

Following the flood of July 1996, a significant quantity of sediment, coming from the catchment areas contiguous to the Saguenay fjord, was discharged in the Baie des Ha! Ha! and the North Arm. To characterize the mode of deposit and the potential for remobilization of these deposits, a series of cores was taken in the fjord using a box corer and a gravity corer during the summers of 1997 and 1998. These cores have been analyzed by the axial tomodensitometer at the Regional Hospital Center of Rimouski. The use of the tomodensitometer in geology allows a nondestructive study of the sample and a qualitative and quantitative evaluation of the density of the sediments, their mode of deposition, and their compaction. The study of the upper 45 cm of sediments shows the presence, in the uppermost layer, of several facies type characteristics of a gravity deposit. This layer rests on an erosional unconformity cut into the surface of the older deposits, themselves of gravity type. One year after the flood, no trace of reworking could be detected in the upper part of the cores. Nevertheless, cores taken in the summer of 1998 show a significant reworking of the superficial sediments in direct relation with bioturbation. No reworking of hydrodynamic origin was observed.Key words: scanography, flood, turbidity currents, sedimentary structures, compaction, bioturbation.

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)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.121
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0010.002
Scholarly communication0.0000.000
Open science0.0010.000
Research integrity0.0010.001
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 head0.008
GPT teacher head0.223
Teacher spread0.215 · 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 designObservational
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

Citations35
Published2002
Admission routes2
Has abstractyes

Explore more

Same venueCanadian Geotechnical JournalSame topicHydrology and Sediment Transport ProcessesFrench-language works237,207