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Record W6998321452

Allostratigraphy of the Cretaceous, Lower Colorado Group in SE Alberta: Tectonic and eustatic controls on depositional cyclicity

2024· article· en· W6998321452 on OpenAlexaboutno aff

Bibliographic record

VenueScholarship@Western (Western University) · 2024
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological formations and processes
Canadian institutionsnot available
Fundersnot available
KeywordsOnlapUnconformityFaciesSedimentary depositional environmentTectonicsTectonic subsidenceForeland basinMarine transgressionSea levelSedimentary rock
DOInot available

Abstract

fetched live from OpenAlex

The Lower Colorado Group is a Cretaceous, shallow marine, clastic succession, 150-200 m thick, deposited in the Western Canada Foreland Basin during the Late Albian and Early Cenomanian (c. 105-100 Ma). High-resolution allostratigraphy based on marine flooding surfaces allowed recognition of four alloformations: Basal Colorado, Joli Fou, Viking, and Westgate, in ascending order. Alloformations can be similarly divided into allomembers and sequences.\nThe Basal Colorado alloformation, comprising five allomembers, thickens southward and records active thrust loading to the south. The overlying Joli Fou and Viking alloformations are broadly sheet-like and record tectonic quiescence, and even uplift of the Cordillera, as suggested by the westward thinning of the Viking alloformation. At this time, depocentres were laterally offset from one another, and progressively shift seaward, to the NE, as a result of very limited accommodation and progressive filling of up-dip accommodation.\nA brief pulse of tectonic loading is inferred from Westgate sequence WCa that is of alluvial facies, and thickens to the SW. Sheet-like, sandy deltaic facies of Westgate sequences WCb to WCe prograde to the NE and suggest tectonic quiescence. The overlying, mudstone-dominated sequences WCf to WCj onlap westward but thicken to the SE. This reflects eustatic rise and subsidence of the intracratonic Williston Basin.\nAbrupt thickness and lateral facies changes in parts of the Joli Fou, Viking and Westgate alloformations define linear belts that suggest syn-depositional fault movement that localized the position of deltas. Faults may be related to deep-seated structures in the Precambrian basement, and may have been active at times of low in-plane stress.\nThe Basal Colorado plus Joli Fou record a long-term (> 1 Myr) tectono-eustatic sea-level rise when the basin was flooded from both north and south, whereas the Viking alloformation records eustatic fall and regression. The Westgate records a second long-term eustatic rise, with transgression from the north. Higher-frequency sea-level cycles of ?10-20 m are superimposed on these long-term cycles, with allomembers and their internal sequences apparently spanning c. 500 and c. 100 kyr, respectively, possibly reflecting long and short orbital eccentricity cycles that modulated climate, driving sea-level change through aquifer eustasy and/or glacio-eustasy.

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 score0.037
Threshold uncertainty score0.074

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0030.003
Science and technology studies0.0010.001
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 head0.038
GPT teacher head0.260
Teacher spread0.222 · 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
Published2024
Admission routes1
Has abstractyes

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