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Record W2799602805 · doi:10.7939/r33t9db98

Controls on organic-rich mudstone deposition: The Devonian Duvernay Formation, Alberta, Canada

2016· article· en· W2799602805 on OpenAlexaboutno aff
Levi J. Knapp

Bibliographic record

VenueUniversity of Alberta Library · 2016
Typearticle
Languageen
FieldEngineering
TopicHydrocarbon exploration and reservoir analysis
Canadian institutionsnot available
Fundersnot available
KeywordsDevonianGeologyDeposition (geology)GeochemistryPaleozoicLate Devonian extinctionPaleontologyCarboniferousStructural basin

Abstract

fetched live from OpenAlex

The Upper Devonian Duvernay Formation of Western Canada is a prolific source rock that in recent years has become an exploration target for shale gas and liquids. Development of the Duvernay Formation has demonstrated the importance of robust models for rock properties such as porosity, permeability, organic richness, and fracturability. Depositional processes and conditions govern the character and distribution of mudstone lithofacies, which are directly linked to variations in rock properties. The depositional and sequence stratigraphic models presented here are based on a detailed sedimentology and stratigraphy study. Twelve lithofacies were characterized based on lithology, sedimentary and biogenic structures, fossil type and abundance, and type and abundance of cement. Significant variation exists between organic-rich lithofacies, indicating that organic-rich mudstones were deposited in variably energetic and oxygenated environments, rather than within persistently anoxic, stagnant bottom waters. Correlation of core descriptions to a network of 759 wells with wireline logs led to the creation of a basin-scale sequence stratigraphic framework with 3 third order sequences. The sequence stratigraphic model shows a strong sea level and basin morphology control on basinal lithofacies. Transgression, and subsequent highstand normal regression in sequence 1 (oldest) resulted in significant platform construction in the northeast side of the basin. Sediments become consistently finer-grained and organic-rich away from the platform. Major transgression at the start of sequence 2 resulted in flooding of the platform and significant upslope trapping of sediments, locally so significant that no sediment reached the platform edge and large zones of non-deposition developed. Lithofacies basinward of these zones are especially clay mineral-poor and organic-rich. A sea level stillstand or lowstand at the base of sequence 3 resulted in progradation of basin-margin facies, reduction in the extent of organic-rich mudstone deposition, and an influx of clay minerals into the basin. The geographic extent of organic-rich, siliceous mudstone deposition was greatest during transgressive and highstand systems tracts. Sustained highstands resulted in increased carbonate sedimentation, which diluted organic matter. Sea level stillstands resulted in progradation of argillaceous sediment, and reduction of TOC values due to dilution and oxygenation.

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 categoriesInsufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Not applicable · Consensus signal: Not applicable
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.633
Threshold uncertainty score0.999

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 communication0.0000.001
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

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 head0.003
GPT teacher head0.139
Teacher spread0.136 · 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

Citations4
Published2016
Admission routes1
Has abstractyes

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