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Record W2909999351 · doi:10.4095/212595

Carboniferous and Permian subsurface stratigraphy, Prince Patrick Island, Northwest Territories, Canadian Arctic

2001· report· en· W2909999351 on OpenAlexaffabout
B. Beauchamp, John Harrison, J. Utting, T A Brent, Stéphanie Pinard

Bibliographic record

Venuenot available
Typereport
Languageen
FieldEarth and Planetary Sciences
TopicGeological Studies and Exploration
Canadian institutionsNatural Resources Canada
Fundersnot available
KeywordsCarboniferousPermianStratigraphyGeologyArcticPaleontologyArchaeologyOceanographyGeographyStructural basinTectonics

Abstract

fetched live from OpenAlex

The Carboniferous and Permian succession of the Sverdrup Basin is extensive in the subsurface of northern Prince Patrick Island of the Canadian Arctic Archipelago, Northwest Territories. The succession is known from a series of seismic profiles and four exploratory wells drilled during the early 1970s. Upper Paleozoic strata are characterized by two broad packages. The lower package comprises Carboniferous to Lower Permian clastic and carbonate rocks truncated by a number of northwest southeast-trending synsedimentary normal faults. The upper package is composed of Middle Permian (Guadalupian) clastic rocks that were deposited during a regime of passive subsidence following the cessation of faulting. These strata are separated from the underlying Lower Permian and Carboniferous succession by a widespread and locally angular unconformity. Eleven upper Paleozoic formations have been identified on Prince Patrick Island: Borup Fiord, Canyon Fiord, Belcher Channel, Nansen, Raanes, Hare Fiord, 'unnamed clastics', Trappers Cove, Sabine Bay, van Hauen, and Trold Fiord. The succession contains eight major unconformities that can be correlated over a significant area. Five of these unconformities were encountered in three of the drilled wells. Three additional unconformities were observed on seismic profiles only. The eight unconformities and the seven transgressive regressive sequences between them have been traced seismically using a series of profiles. The ages of these sequences are Serpukhovian(?), Bashkirian Kasimovian, Gzhelian Sakmarian, Sakmarian Artinskian, Kungurian, Roadian Wordian and Capitanian(?). The Carboniferous and Permian geological history of Prince Patrick Island includes a complex succession of events whereby tectonic pulses, as evidenced by brittle deformation, alternated with episodes of tectonic quiescence and passive subsidence. Climatic conditions evolved from warm and relatively arid during the Bashkirian Sakmarian interval to increasingly cooler during the Artinskian Capitanian(?). More humid conditions were also established during the Kungurian. A major river system fed the Prince Patrick area with large amounts of clastic material during the Artinksian Guadalupian interval. The current geological setting of the area suggests the presence of many unexplored oil and gas plays. Unfortunately, the succession lies too deeply in the subsurface to envision any mineral exploration effort in the future.

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)0.001
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 score0.011
Threshold uncertainty score0.082

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.004
Science and technology studies0.0040.001
Scholarly communication0.0010.000
Open science0.0010.001
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 head0.022
GPT teacher head0.210
Teacher spread0.188 · 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

Citations25
Published2001
Admission routes2
Has abstractyes

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