MétaCan
Menu
← Back to cohort
Record W7133013081

Litho-, Chrono-and allostratigraphy of the Santonian to Campanian Milk River and Eagle formations in southern Alberta and north-central Montana: implications for differential subsidence in the western interior foreland baseland

2002· dissertation· W7133013081 on OpenAlexfundaboutno aff
Tobias Payenberg

Bibliographic record

VenueTSpace · 2002
Typedissertation
Language
FieldEarth and Planetary Sciences
TopicPaleontology and Stratigraphy of Fossils
Canadian institutionsnot available
FundersNatural Sciences and Engineering Research Council of CanadaUniversity of TorontoGovernment of Ontario
KeywordsMarine transgressionForeland basinEagleClastic rockSequence (biology)Sedimentary rockCretaceousSubsidenceUnconformity
DOInot available

Abstract

fetched live from OpenAlex

The Santonian to Campanian succession of southern Alberta and northern Montana contains the Milk River/Eagle clastic wedge, encased in marine Colorado and Claggett/Pakowki shales. Litho- and chronostratigraphic analysis across the international border showed that the Santonian Telegraph Creek Member/Formation and the Virgelle and Deadhorse Coulee members are in lithostratigraphic continuity, and of similar age along the paleoshoreline. The Earliest Campanian saw clastic sedimentation of the Upper Eagle Member in north-central Montana, while a hiatus of up to 2.5 Ma developed in southern Alberta around Writing-On-Stone Provincial Park. Only the Pakowki/Claggett transgression during the Early Campanian was again synchronous across the study area. The Santonian Virgelle shoreline is marked by a strong dominance of storm generated sedimentary structures in an unusually thick shoreface succession exceeding 30 m. Campanian Upper Eagle sedimentation took place in a more restricted, deltaic environment that was sourced from the southwest. Based on an allostratigraphic approach, high-resolution sequence analysis enabled the subdivision of the study interval into seven allomembers. The first three allomembers, Virgelle 1, 2 and 3, are each seaward stepping from another. Following a regional transgression was the deposition of the Upper Eagle A, B and C allomembers, also in seaward stepping shingles. Upper Eagle D Allomember is a transgressive unit topped by the regional “Eagle Shoulder” sequence boundary. The hiatus developed in southern Alberta during the Earliest Campanian is reflected in the distribution of the Upper Eagle allomembers. Projection of the Upper Eagle allomembers onto structural elements of the Sweetgrass Arch shows the coastal sandstones curving around the Kevin Sunburst Dome element of the Sweetgrass Arch and paralleling its structural contours. Despite often cited basement control for the Sweetgrass Arch, aeromagnetic data does not show any direct correlation of basement lineaments with the anticlinal crest of the Kevin Sunburst Dome. However, a magnetically heterogeneous block of crest underneath the Kevin Sunburst Dome, surrounded by very highly magnetic crustal material, might have buckled under stress due to different rheological properties. This could explain the up and down movement observed in the hiatus and distribution patterns of the Milk River/Eagle interval.

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 score0.380
Threshold uncertainty score0.765

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.001
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 head0.018
GPT teacher head0.256
Teacher spread0.238 · 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
Published2002
Admission routes2
Has abstractyes

Explore more

Same venueTSpace→Same topicPaleontology and Stratigraphy of Fossils→French-language works237,207→