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Record W3177982817 · doi:10.1029/2021tc006764

Tectonic Growth of the Late Paleozoic‐Middle Mesozoic Northwestern Margin of Laurentia and Implications for the Farewell Terrane: Stratigraphic, Structural, and Provenance Records From the Central Alaska Range

2021· article· en· W3177982817 on OpenAlexaboutno aff
Brandon Keough, Kenneth D. Ridgway

Bibliographic record

VenueTectonics · 2021
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsnot available
FundersU.S. Geological Survey
KeywordsTerraneGeologyLaurentiaPaleontologyPaleozoicPermianOrdovicianProvenancePassive marginDevonianMesozoicRiftTectonicsStructural basin

Abstract

fetched live from OpenAlex

Abstract Analysis of upper Paleozoic‐Jurassic strata in the central Alaska Range provides new insights into the following: the configuration of Late Triassic‐Jurassic depocenters along the northwestern Laurentian margin, the late Paleozoic paleogeographic position of the Farewell terrane, and the timing of accretion of the Farewell terrane to the Laurentian margin. Results from geologic mapping, stratigraphic analysis, and U‐Pb detrital zircon geochronology document two juxtaposed Paleozoic‐Jurassic stratigraphic assemblages. The Southern package consists of Permian‐Middle Triassic submarine fan strata and Upper Triassic pillow basalts that can be correlated with the Farewell terrane of the western Alaska Range. This package yields Ordovician‐Silurian and Late Pennsylvanian‐Early Permian detrital zircons linked to the Alexander and Wrangellia terranes. This detrital connection suggests that the Farewell terrane most likely collided with the Insular terranes in the paleo‐Pacific basin during the late Paleozoic. The Northern package, in contrast, consists of Upper Triassic‐Jurassic submarine fan strata deposited along the northwestern margin of Laurentia. An abundance of Neoproterozoic and early Paleozoic detrital zircons suggests recycling of Caledonian and Baltican zircons from the Ellesmerian clastic wedge of northwestern Canada. An influx of Late Triassic‐Early Jurassic detrital zircons in Upper Jurassic strata of the Northern package records the development of Mesozoic arc magmatism along the continental margin. Our findings document deformation consistent with latest Jurassic‐earliest Cretaceous accretion of the Farewell terrane to the Laurentian margin. Our results also suggest that the Farewell terrane may underlie much of the central Alaska Range, and played an important role in the construction of the northern Cordillera.

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 score0.160
Threshold uncertainty score0.319

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.000
Science and technology studies0.0010.000
Scholarly communication0.0010.000
Open science0.0000.000
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 head0.014
GPT teacher head0.194
Teacher spread0.180 · 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

Citations7
Published2021
Admission routes1
Has abstractyes

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