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Record W2982273234 · doi:10.4095/295194

Organic geochemistry of petroleum hydrocarbons in Middle to Upper Devonian outcrop samples from Mackenzie Plain area

2014· report· en· W2982273234 on OpenAlexaff
Chunqing Jiang, Leanne J. Pyle, L P Gal

Bibliographic record

Venuenot available
Typereport
Languageen
FieldEngineering
TopicHydrocarbon exploration and reservoir analysis
Canadian institutionsNatural Resources Canada
Fundersnot available
KeywordsOutcropDevonianGeologyGeochemistryOrganic geochemistryCoastal plainPetroleum geochemistryPetroleumMineralogySource rockPaleontologyKerogen

Abstract

fetched live from OpenAlex

Rock-Eval analysis and hydrocarbon biomarker characterization have been carried out on Middle to Upper Devonian oil-stained outcrop samples collected from the Mackenzie Plain area. While an interpretation of the available organic geochemical results supports the current understanding that the Devonian Canol Formation and Bluefish Member (basal Hare Indian Formation) shales may have been the major source rocks to most oil accumulations in Middle to Upper Devonian reservoirs, an effective older source rock system is proposed to have sourced some of the oil occurrences in the area. Except for extremely organic-lean samples in which major hydrocarbon components (e.g. paraffin wax) might be mainly from contamination, organic-rich outcrop samples display hydrocarbon signatures of moderate to heavy biodegradation with their normal alkanes being partially or totally removed. Source facies parameters such as the ratios of dibenzothiophene over phenanthrene and pristane over phytane indicate their major source rocks to be shale rather than carbonate. The sterane compositions suggest most of the oil occurrences in the area are derived from either Canol Formation or Bluefish Member shale or both. Most of the oil stains also contain a high relative abundance of arylisoprenoids, a type of aromatic biomarkers known to be abundant in Devonian shales, including Canol and Bluefish units. The distribution pattern of tri-, tetra- and pentacyclic terpanes seems to be diagnostic in distinguishing the source contribution of Canol Formation from Bluefish Member. Bluefish shale is likely the main source rock for oil occurrences in the Hume Formation limestone in the Mackay Range area, in the Ramparts Formation limestone at Powell Creek, and in the Imperial Formation sandstone at Katherine Creek. In contrast, oil present in the Fort Norman Formation dolostone at Imperial Anticline and in the Imperial Formation dolostone at Prohibition Creek have a terpane composition closer to that of Norman Wells oil and Canol shale, suggesting that Canol shale is their main source rock. The apparent high oil quality (e.g., saturated fraction dominated by C13 to C18 n-alkanes) of an outcrop bitumen sample collected at the Canol-Imperial Formation contact in the Imperial River area provides strong evidence of dynamic oil expulsion, migration and accumulation within the Canol petroleum system in the area. The C29-dominant sterane distribution feature in some Ramparts Formation limestone samples from Powell Creek and Mountain River II site suggests that there might have been an active Precambrian source rock system contributing to oil accumulations in the Mackenzie Plain area.

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: Observational
GenreCandidate signal: Other · Consensus signal: none
Teacher disagreement score0.947
Threshold uncertainty score0.104

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.001
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

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 head0.028
GPT teacher head0.235
Teacher spread0.207 · 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
GenreOther

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

Citations1
Published2014
Admission routes1
Has abstractyes

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