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Record W2787913691

The Upper Devonian-Lower Mississippian Bakken Formation of west-central Saskatchewan: stratigraphic architecture and sequence stratigraphy of a conventional heavy oil reservoir

2017· article· en· W2787913691 on OpenAlexaffvenueabout
Luc E. Chabanole, Luís A. Buatois

Bibliographic record

VenueBulletin of Canadian Petroleum Geology · 2017
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological formations and processes
Canadian institutionsUniversity of Saskatchewan
Fundersnot available
KeywordsGeologySiltstoneMarine transgressionProgradationDevonianPaleontologyIsopach mapPennsylvanianOil shaleFluvialSequence stratigraphyGeochemistrySedimentary depositional environmentFaciesStructural basin
DOInot available

Abstract

fetched live from OpenAlex

Abstract The Bakken Formation (Upper Devonian-Lower Mississippian) of western Saskatchewan has lower and upper members dominated by black shales and a heterolithic middle member, similar to southeastern Saskatchewan and North Dakota. However, the middle member in western Saskatchewan contains fine-grained sandstone where porosity and permeability values commonly exceed 25% and 1 Darcy respectively that are absent in southeastern Saskatchewan and North Dakota. Although focus has been in southeastern Saskatchewan and North Dakota, the Bakken Formation of west-central Saskatchewan has conventionally produced heavy gravity oil (API approximately 12 degrees) since the 1950s using vertical wells. The sequence-stratigraphic framework of the Bakken Formation of west-central Saskatchewan includes deposition under open-marine and marginal-marine conditions. Open-marine black shales were deposited during late-stage transgression (TST1) and progradation of offshore siltstones during the subsequent highstand systems tract (HST). Fine-grained sandstone, siltstone, and mudstone showing evidence of tidal influence was deposited during a falling-stage systems tract (FSST), initiated under forced-regressive conditions. Increased fluvial influence and dilution of normal marine salinity established marginal-marine conditions, evidenced by the low bioturbation index (BI: 0−2). Subsequent transgression (TST2) led to increased marine influence, reflected in a sudden increase in biogenic activity (BI: 4−5). Offshore siltstone and black shale were deposited through continued transgression (TST2) resulting in the re-establishment of open-marine conditions. Preserved thickness of the Bakken Formation in west-central Saskatchewan has been affected by post-Mississippian erosion during the creation of the sub-Cantuar drainage network, which was later filled by Lower Cretaceous clastics. The Bakken middle marginal-marine interval in west-central Saskatchewan differs from that in southeastern Saskatchewan. Fine-grained sandstones associated with tidal channels in west-central Saskatchewan comprise a reservoir characterized by porosity and permeability values that commonly exceed 25% and 1 Darcy, respectively. In contrast, in southeastern Saskatchewan, the Bakken Formation produces from a dolomitized silty sandstone where low porosity and permeability values have led to the widespread use of unconventional exploitation techniques to produce economically.

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: Empirical · Consensus signal: Empirical
Teacher disagreement score0.259
Threshold uncertainty score0.522

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.002
Science and technology studies0.0010.001
Scholarly communication0.0010.000
Open science0.0000.001
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0030.000

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 head0.013
GPT teacher head0.206
Teacher spread0.193 · 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

Citations2
Published2017
Admission routes3
Has abstractyes

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