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Record W2181493996

The Graminia-Blueridge of Northeast Alberta: A New Devonian Subcrop Bitumen Play

2013· article· en· W2181493996 on OpenAlexaboutno aff
Kent R. Barrett

Bibliographic record

Venuenot available
Typearticle
Languageen
FieldEngineering
TopicHydrocarbon exploration and reservoir analysis
Canadian institutionsnot available
Fundersnot available
KeywordsGeologyDolomiteCarbonateCalciteDolomitizationDiagenesisDevonianGeochemistryMeteoric waterCretaceousStylolitePorosityCarbonate rockUnconformityDissolutionMineralogySedimentary rockPaleontologyGeotechnical engineeringChemistryStructural basin
DOInot available

Abstract

fetched live from OpenAlex

Summary The Upper Devonian Blueridge and Graminia Formations contain a significant bitumen resource that has been the focus of recent drilling by Laricina Energy Ltd in the Germain area (T 84 R 22W4) of northeastern Alberta. The Graminia and Blueridge Formations of the Winterburn Group are peritidal carbonates that are distinguished by the higher argillaceous content of the former. They have a complex diagenetic history which includes late Devonian to early Mississippian dolomitization and early Cretaceous(?) fresh water leaching. This was quickly followed by oil migration and subsequent biodegradation to bitumen. Oil was trapped along the up-dip erosional subcrop by overlying Cretaceous shales. Calcite is more soluble than dolomite under surface conditions. Exposing dolomitic strata to fresh meteoric water will result in the preferential leaching of any residual calcite-rich material. Intraparticle porosity develops within carbonate grainstones due to preferential leaching of coarser grains over the finer matrix material. This is sometimes referred to as pinpoint vug porosity. The less soluble dolomite matrix formed a rigid framework preventing the wholesale dissolution of the carbonate bed. Some beds develop high porosity and become conduits for the flow of large volumes of fresh water. Under these conditions, cavernous porosity was created. These caverns are up to at least one meter high and contain a variety of filling materials including angular dolomitic breccias, insoluble residue from carbonate dissolution and Cretaceous(?) mudstones. Graminia and Blueridge reservoirs are typically greater than 20% porosity and commonly exceed 30%. Permeabilities typically are greater than 200 mD and sometimes range up to several darcies. Permeability is augmented by numerous sub-vertical fractures. The gross bitumen saturated interval is greater than 30m thick. Its oil saturation is greater than 80%, supporting the theory that the Graminia-Blueridge is an oil wet reservoir. The stratified nature of the reservoir will create challenges in developing a bitumen extraction strategy as it may preclude the use of horizontal wells. Possible application of alternative thermal and solvent applications is being considered. Cores from Laricina’s recent drilling program will be used to show the nature of the GraminiaBlueridge reservoir development and bitumen resource. Core from at least one cave interval will be displayed.

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)0.000
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.107
Threshold uncertainty score0.216

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.001
Science and technology studies0.0070.003
Scholarly communication0.0030.000
Open science0.0010.002
Research integrity0.0000.001
Insufficient payload (model declined to judge)0.0090.001

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 head0.007
GPT teacher head0.192
Teacher spread0.185 · 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 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

Citations0
Published2013
Admission routes1
Has abstractyes

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