MétaCan
Menu
Back to cohort
Record W2011539280 · doi:10.2475/02.2007.01

The Middle Ordovician to Early Silurian voyage of the Dashwoods microcontinent, West Newfoundland; based on new U/Pb and 40Ar/39Ar geochronological, and kinematic constraints

2007· article· en· W2011539280 on OpenAlexafffundabout
A. G. Brem, Shoufa Lin, Cees R. van Staal, D. W. Davis, V J McNicoll

Bibliographic record

VenueAmerican Journal of Science · 2007
Typearticle
Languageen
FieldMedicine
TopicInfectious Diseases and Tuberculosis
Canadian institutionsUniversity of TorontoUniversity of WaterlooGeological Survey of Canada
FundersNatural Sciences and Engineering Research Council of CanadaUniversity of Toronto
KeywordsGeologyOrdovicianSinistral and dextralPaleontologyTectonicsFault (geology)OrogenyPegmatiteSubductionSeismology

Abstract

fetched live from OpenAlex

The Dashwoods microcontinent is an important tectonic segment in the peri-Laurentian setting of the Newfoundland Appalachians. In order to better understand the tectonic history of Dashwoods during the Ordovician Taconic orogeny, we have undertaken field mapping, microscopic studies, and U-Pb and ^40^Ar/^39^Ar geochronological studies along the northern (Little Grand Lake Fault; LGLF) and western (Baie Verte Brompton Line - Cabot Fault Zone; BCZ) boundaries. Oblique-dextral ductile deformation in the BCZ occurred from late Middle Ordovician into the Early Silurian, based on the presence of a late syn-tectonic pegmatite dike (455 ± 12 Ma) and a foliated granodiorite sheet (445.8 ± 0.6 Ma). Deformation is coeval with oblique-sinistral accretion along the eastern margin of Dashwoods, which means that Dashwoods and its Notre Dame Arc had a southward translation with respect to the Laurentian margin and the then-present Iapetus Ocean during the Late Ordovician. Dextral movement along the BCZ continued after the collision of Dashwoods with the Laurentian margin. Deformation along the Little Grand Lake Fault is bracketed between 463 ± 5 Ma and 440 ± Ma. These ages combined with other geological arguments indicate that motion probably took place during the Late Ordovician to earliest Silurian contemporaneous with the southward translation of Dashwoods. A possible explanation is that the Snooks Arm arc moved independently from and faster southwards than the Notre Dame Arc with its Dashwoods infrastructure, thereby underthrusting the Dashwoods along the Little Grand Lake Fault. Our new U-Pb geochronological data, including a muscovite granite (463 ± 5 Ma), a schistose muscovite granite (459 ^+17^/~-21~ Ma), and a tectonized tonalite (458 ± 20 Ma), add to the geochronological database of the voluminous second phase of the Notre Dame Arc. Additionally, in all-but-one of our U-Pb samples, inherited grains of Mesoproterozoic (circa 1.0 Ga) age have been obtained. Their regional presence fortifies the possible relationship of the Dashwoods microcontinent with the Long Range Inlier in western Newfoundland. Furthermore, it introduces a potential link with the Blair River Inlier in Cape Breton Island.

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 score0.106
Threshold uncertainty score0.213

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 communication0.0020.000
Open science0.0000.001
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 head0.010
GPT teacher head0.259
Teacher spread0.249 · 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
Published2007
Admission routes3
Has abstractyes

Explore more

Same venueAmerican Journal of ScienceSame topicInfectious Diseases and TuberculosisFrench-language works237,207