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Record W2795909752 · doi:10.1130/abs/2018ne-310665

HOW GEOLOGICAL MAPPING, PETROLOGICAL STUDIES, AND U-PB (ZIRCON) DATING LED TO RECOGNITION OF SEPARATE NEOPROTEROZOIC, CAMBRIAN, ORDOVICIAN, AND SILURIAN CONVERGENT MARGIN MAGMATISM IN WESTERN CAPE BRETON ISLAND, NOVA SCOTIA, CANADA

2018· article· en· W2795909752 on OpenAlexaboutno aff
Chris E. White, Sandra M. Barr, Deanne van Rooyen, Jonathan M. Shute, Travis McCarron, Gabriel Sombini dos Santos

Bibliographic record

VenueAbstracts with programs - Geological Society of America · 2018
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsnot available
Fundersnot available
KeywordsGeologyTerraneZirconPlutonVolcanic rockGeochemistryOrdovicianPaleontologyVolcanoTectonics

Abstract

fetched live from OpenAlex

The western part of the Cape Breton Highlands of Nova Scotia has been recognized for decades as an area of complex and enigmatic relations among metamorphic and igneous rocks of poorly constrained Neoproterozoic to Devonian ages. Recent mapping resulted in a revised geological map of the area, with units constrained by new U-Pb (zircon) ages. In addition, petrological studies have led to new interpretations of tectonic setting, and clarified the relationship of the rocks west and east of the mylonitic Western Highlands shear zone. The area west of the shear zone (Cheticamp-Jumping Brook belt) includes Neoproterozoic metasedimentary rocks and a granitoid suite formed in a continental margin subduction zone. These rocks are linked to the Bras d'Or terrane of central Cape Breton Island, as well as to poorly preserved units of similar age in the Crippleback Intrusive Suite of the Exploits terrane in Newfoundland. These older rocks are in faulted contact with Cambrian sulphide-bearing back-arc sedimentary and basaltic rocks of the Jumping Brook Metamorphic Suite and intruded by large Ordovician tonalitic and dioritic arc-type plutons, possibly correlative with the Victoria Lake Supergroup and associated plutonic rocks in the Exploits terrane of Newfoundland. Previously unrecognized but widespread Silurian dioritic to granitic rocks formed in a volcanic-arc setting are associated with the Neoproterozoic rocks. The youngest rocks are a widespread cover sequence of ca. 374-372 Ma bimodal volcanic and associated sedimentary rocks and related gabbroic and granitic plutons. The plutons are undeformed and cut the Western Highlands shear zone, thus constraining the timing of juxtaposition of the Cheticamp-Jumping Brook belt west of the shear zone with the Ordovician(?)-Silurian metasedimentary, amphibolitic, and orthogneissic rocks of the Pleasant Bay Complex (PBC) east of the shear zone. The PBC is intruded by abundant Devonian S- and A-type granitoid rocks. Chemical characteristics and ages of amphibolitic and orthogneissic rocks in the PBC indicate that they formed in a mid-Silurian rifted arc. The documentation of arc-related Neoproterozoic, Cambrian, Ordovician, and Silurian rocks strengthens the evidence of correlation of the Aspy terrane with the Ganderian Exploits terrane of Newfoundland and New Brunswick.

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 score0.326
Threshold uncertainty score0.993

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0010.000
Bibliometrics0.0000.001
Science and technology studies0.0000.002
Scholarly communication0.0000.000
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 head0.023
GPT teacher head0.226
Teacher spread0.203 · 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".

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Citations0
Published2018
Admission routes1
Has abstractyes

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