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Record W60180786

Sedimentology and Allostratigraphy of the Cardium Formation (Turonian-Coniacian) in southern Alberta, and equivalent strata in northern Montana

2012· article· en· W60180786 on OpenAlexaboutno aff
Joel A. Shank

Bibliographic record

VenueScholarship@Western (Western University) · 2012
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicPaleontology and Stratigraphy of Fossils
Canadian institutionsnot available
Fundersnot available
KeywordsSedimentologyGeologyPaleontologyArchaeologyGeochemistryGeography
DOInot available

Abstract

fetched live from OpenAlex

The Turonian-Coniacian Cardium Formation of southern Alberta consists of marine sandstone and mudstone, deposited in a foreland basin over ~2.3 m.y. The formation thins from 150 m in the western foredeep to 50 m 350 km to the east. Correlation of 10 regional flooding surfaces in >1200 well logs and 25 outcrops provides an allostratigraphic framework. Mapping of two previously-unrecognized erosion surfaces (E5.2 and E5.5) reveals additional complexity within sandstone of the Raven River Member.\nFacies successions coarsen upwards from thinly-bedded and bioturbated mudstone, to heterolithic facies (either bioturbated or bedded), to clean sandstone. Where conglomerate unconformably overlies this succession, the base of the conglomerate marks a regional erosion surface. A tabular geometry, and wave-formed sedimentary structures even in distal settings, indicate deposition on a very low gradient shelf within the mud accommodation envelope (~70 m), and at times, within effective wave-base for sand (~40 m).\nIsopach maps reveal two pulses of isostatic subsidence that were separated by a period of tectonic quiescence. The locus of flexural subsidence shifted southward by >200 kilometres in <1.2 m.y. during the first pulse of subsidence, indicating a southward shift in the position of the active load. Basement structures, including the Vulcan Low, Bow Island Arch, Red Deer High, and faults, caused differential subsidence and localized thickness changes in several allomembers.\nThe relative sea-level history of the Cardium Formation is characterized by two major relative sea-level falls (Late Turonian and Early Coniacian), separated by a major transgression (latest Turonian, Niobrara transgression). Higher-frequency relative sea-level changes are superimposed on this long-term curve.\nThree regressive-transgressive cycles in the Cardium Formation can be correlated to similar cycles in the Bohemian Basin of the Czech Republic, based on biostratigraphic evidence, indicating a probable eustatic mechanism. In combination with previous studies, flooding surfaces that define Cardium allomembers have now been correlated >900 kilometres along strike, ~300 kilometres offshore, and between depocentres, suggesting a eustatic mechanism. Facies relationships across flooding surfaces suggest that eustatic fluctuations had a magnitude of ~12 m and a frequency of ~250 k.y., and are therefore best explained by glacioeustasy.

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 score0.061
Threshold uncertainty score0.122

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 studies0.0010.001
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 head0.047
GPT teacher head0.256
Teacher spread0.209 · 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

Citations4
Published2012
Admission routes1
Has abstractyes

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