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Record W2110864802 · doi:10.4138/1970

Mafic intrusions on Campobello Island: implications for New Brunswick - Maine correlations

2001· article· en· W2110864802 on OpenAlex
Malcolm McLeod, Ron K. Pickerill, R. Dan Lux

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

affAt least one author lists a Canadian institution in the pinned OpenAlex snapshot.
venuePublished in a venue whose home country is Canada.
aboutThe title or abstract carries a Canadian signal from the geographic lexicon.

Bibliographic record

VenueAtlantic Geology · 2001
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsUniversity of New Brunswick
Fundersnot available
KeywordsGeologyMaficFelsicOrdovicianMetamorphismVolcanic arcIsland arcAndesitesGeochemistryPaleozoicBasementVolcanic rockContinental arcPaleontologySubductionVolcanoAndesiteTectonicsArchaeology

Abstract

fetched live from OpenAlex

Late Ordovician through Early Devonian units of the Passamaquoddy Bay area are interpreted to represent sequences that evolved in arc and back-arc environments. The main elements of the arc are exposed on Campobello Island and include a predominantly felsic volcanic sequence to the northeast, a sequence of intercalated turbidite and mafic volcanic rocks to the southwest, and matic dyke swarms throughout. Petrographic. geochemical, and 40Ar/39Ar studies of these rocks record episodic deformation and varying degrees of metamorphism up to lower amphibolite facies, and a protracted history of mafic magma injection from a similar source beginning in the Early Silurian. These features, combined with stratigraphic relationships and overall structural patterns, indicate a rapid transition from felsic- to mafic-dominated magmatism accompanied by radical changes in the depositional regime in the arc with time, and exposure of progressively deeper crustal levels towards the northeast within the arc.
 
 Review of the assignment of other units in the Passamaquoddy Bay region to major tectonostratigraphic bells north of Campobello Island clarifies regional correlations and provides possible additional links to Neoproterozoic basement in the area.
 
 RÉSUMÉ
 Les unités de l'Ordovicien superieur au Dévonicn inférieur du secteur de la baie Passamaquoddy sont interprétées comme des unités représentatives de séquences ayant évolué dans des environnements d'arc et d'arriére-arc. Les principaux éléments de de l'arc affleurent sur l'ile Campobello et component une séquence principalcment volcanofelsique au nord-est. une sequence volcanomafique/turbiditique intercalée au sud-ouest et des groupes de filons mafiques un peu panout. Des études pétrographiques. géochimiques et 40Ar/39Ar de ces roches rélèvent une déformation épisodique et des degrés divers de métamorphisme jusqu'au faciès amphibolique infèrieur, ainsi que des antécédents prolongés d'injection de magma mafique d'une source similairc à partir du Silurien inferieur. Ces particulierités conjuguécs aux relations stratigraphiques et aux configurations slructurales générates, révèlent une transition rapide d'un magmatisme à prédominance mafique a un magmatisme à prédominance mafique accompagné de changements spectaculaires dans te régime de sédimentation à l'intérieur de l'are avec le temps, ainsi qu'un affleurement de niveaux crustaux progressivement plus profonds vers le nord-est a l'intcrieur de l'are.
 
 L'examen de l'affectation des autres unités dans la region de la baie Passamaquoddy aux principals structures teconostratigraphiques au nord de l'ile Campobello clarifie les correlations régionalcs et foumit des liens supplémentaires possibles avec le socle du Protéroique supérieur du secteur.
 
 Traduit par la rédaction

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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 categoriesInsufficient payload (model declined to judge)
Consensus categoriesInsufficient payload (model declined to judge)
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.132
Threshold uncertainty score0.999

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0140.001

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 head0.017
GPT teacher head0.225
Teacher spread0.208 · 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