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Record W6998496630

Allostratigraphy of the Lower Colorado Group (Cretaceous) in south-west Alberta

2021· article· en· W6998496630 on OpenAlexaboutno aff

Bibliographic record

VenueScholarship@Western (Western University) · 2021
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological formations and processes
Canadian institutionsnot available
Fundersnot available
KeywordsOutcropFaciesSedimentary depositional environmentAlluviumGroup (periodic table)Structural basinForeland basinTectonics
DOInot available

Abstract

fetched live from OpenAlex

Clastic, upper Albian-lower Cenomanian strata were deposited in a low-accommodation backbulge depozone of the Western Canada Foreland Basin in SW Alberta. These strata are lithologically very heterogeneous and encompass a spectrum of depositional environments along an alluvial to offshore transect. These rocks are assigned, in subsurface, to the Lower Colorado Group, and in outcrop to the upper Blairmore Group. Lithological heterogeneity, as a result of rapid lateral facies changes, resulted in diverse nomenclature that obscured genetic relationships between time-equivalent strata. The present study integrates wireline log, core, and outcrop data to establish a high-resolution allostratigraphic framework which allowed recognition of the Basal Colorado, Joli Fou, Viking and Westgate alloformations, in ascending order. Each alloformation comprises several allomembers and parasequences. The Basal Colorado alloformation is a NE thinning wedge that progressively onlaps lower Albian Mannville Group strata. Deposition took place in a brackish-water embayment open to the south. Basal Colorado strata correlate with the Lynx Creek Member of the Mill Creek Formation in outcrop. The Joli Fou and Viking alloformations have a broadly sheet-like geometry. Both alloformations comprise three allomembers, composed of a complex array of river-dominated and mixed-influence deltaic successions. The location of successive deltas was strongly influenced by differential compaction of underlying deltas. Sandstone-rich Joli Fou rocks pass northward into offshore mudstone. To the south and west, marine Joli Fou and Viking deposits grade laterally into alluvial facies. Only the upper part of the Westgate alloformation extends into SW Alberta. Tectonic tilting is indicated by the lowermost (alluvial) and uppermost (marine) Westgate parasequences, which are SW and NE thickening wedges, respectively. Paleo-valleys, typically ~20 m deep, are incised into the top surface of most allomembers. Different examples of valley incision and fill can be attributed to both sea-level changes, and also to climatically-controlled changes in the sediment load to discharge ratio. Two pulses of thrust-induced loading and a long term (>1 myr) eustatic cycle provided the overall control on stratal architecture, whereas climate-controlled cycles in the ~400 and 100 kyr band exerted an important control on the development of allomembers and parasequences. Eustatic changes are estimated to have been ~20 – 30 m.

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 score0.074
Threshold uncertainty score0.149

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.002
Science and technology studies0.0010.000
Scholarly communication0.0010.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0020.000

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 head0.047
GPT teacher head0.244
Teacher spread0.197 · 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
Published2021
Admission routes1
Has abstractyes

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