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Record W2328225848 · doi:10.1139/cjes-2012-0177

Insights into the Phanerozoic tectonic evolution of the northern Laurentian margin: detrital apatite and zircon (U–Th)/He ages from Devonian strata of the Franklinian Basin, Canadian Arctic Islands

2013· article· en· W2328225848 on OpenAlexaffvenueabout
Owen A. Anfinson, Andrew Leier, Keith Dewing, Bernard Guest, Daniel F. Stöckli, Ashton F. Embry

Bibliographic record

VenueCanadian Journal of Earth Sciences · 2013
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological Studies and Exploration
Canadian institutionsGeological Survey of CanadaUniversity of Calgary
Fundersnot available
KeywordsGeologyLaurentiaZirconDevonianPaleontologyOrogenyTerraneSedimentary depositional environmentPaleozoicLate Devonian extinctionStructural basinTectonicsCarboniferous

Abstract

fetched live from OpenAlex

Middle to Upper Devonian strata of the Franklinian Basin in the Canadian Arctic contain a rich record of Phanerozoic tectonic events along the northern margin of Laurentia. We report detrital thermochronometric zircon (U–Th)/He ages (ZHe; number of aliquots, n = 72) and apatite (U–Th)/He ages (AHe; n = 38) from these Paleozoic strata in an effort to better understand the sediment source regions and the exhumation history of the basin. Detrital ZHe ages are older than corresponding stratigraphic ages and were not reset during subsequent burial, thus constraining both maximum burial depths (<7 km) within the basin and source terrane thermal–tectonic evolution. Paleocurrent data, sediment composition, ε Nd values and detrital zircon U–Pb ages from previous studies indicate Middle to Upper Devonian strata of the Franklinian Basin are derived from two principal sediment source regions, the East Greenland Caledonides and a northern continental landmass (referred to as Crockerland). However, ZHe ages indicate these two distinctly different source regions experienced coeval exhumation in the Silurian Period. ZHe ages from Crockerland-derived sediment provide evidence that this landmass, which collided with northern Laurentia during the Ellesmerian Orogeny, was associated with the Caledonian Orogen. AHe ages from Middle to Upper Devonian strata are younger than depositional ages, indicating the AHe ages are at least partially reset since deposition and hence record information about exhumation of the strata and not the sediment source region. Dispersion of AHe single-grain ages from Middle Devonian strata along the southeastern margin of the basin suggest complex initial single-grain characteristics and may indicate long residence time in the He partial retention zone. AHe ages from Upper Devonian samples from the western margin of the basin are also dispersed but indicate the region experienced protracted exhumation from 330 to 190 Ma during early stages of Sverdrup Basin development. AHe ages from Middle Devonian samples from the western margin of the basin suggest two potential periods of prolonged exhumation in Early Cretaceous (Valanginian to Aptian) and Late Cretaceous (Campanian) times. These ages partially coincide with regional erosional or nondepositional events followed by deposition of major clastic units in the adjacent Sverdrup Basin.

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 distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation 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 score0.107
Threshold uncertainty score0.758

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0010.001
Scholarly communication0.0000.000
Open science0.0010.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

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 head0.011
GPT teacher head0.172
Teacher spread0.161 · 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 teacher head, 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

Citations19
Published2013
Admission routes3
Has abstractyes

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