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Record W3000518368 · doi:10.11575/prism/37449

Structure, metamorphism, and mica thermochronology across the interface between the Purcell Anticlinorium and the Kootenay Arc, Omineca Belt, southeastern British Columbia

2020· dissertation· en· W3000518368 on OpenAlexaboutno aff
Nicole A. Rioseco

Bibliographic record

VenuePRISM (University of Calgary) · 2020
Typedissertation
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsnot available
Fundersnot available
KeywordsThermochronologyMetamorphismGeologyArc (geometry)MicaGeochemistryPaleontologyZirconEngineering

Abstract

fetched live from OpenAlex

The Purcell Anticlinorium (PA) and the Kootenay Arc (KA) represent two major tectonic domains within the southern Omineca belt of the Canadian Cordillera, that are characterized by contrasting structural, metamorphic, and thermochronological histories. Rocks in the core of the PA preserve a Proterozoic phyllitic cleavage (S1). The KA is a polydeformed region in which the dominant fabric (S2) developed during the Early Cretaceous. Both S1 in the PA and S2 in the KA are overprinted by a D3 spaced cleavage and associated crenulation lineations ascribed to later stages of the Cordilleran orogeny. The structural boundary between the KA and the PA is taken as the easternmost occurrence of S2. Peak regional metamorphic conditions in the PA reached biotite grade in the Proterozoic. The KA experienced Early Cretaceous Barrovian metamorphism, with metamorphic grade decreasing eastward from sillimanite + K-feldspar zone to biotite zone towards the PA. The two diachronous domains of biotite grade metamorphism converge in the vicinity of the structural interface. The PA preserves K-Ar and 40Ar/39Ar dates in mica between 1318 and 214 Ma and 837 and 240 Ma, respectively. These dates result from disturbed age spectra, and it is unlikely that they reflect true cooling ages. The temporal and spatial scatter of these dates is interpreted to reflect partial resetting following initial cooling in the Proterozoic, due to some combination of Neoproterozoic and Paleozoic sedimentation, Cordilleran tectonic thickening, and Cordilleran magmatism. In the KA, 40Ar/39Ar dates that range from 139 to 55 Ma are interpreted as cooling ages. They span the interval between the time of metamorphism, magmatism, and final exhumation. The Proterozoic through Mesozoic K-Ar and 40Ar/39Ar cooling dates in the PA indicate that since the Proterozoic, the region was never sufficiently buried to uniformly reset mica cooling dates. It is proposed that the interface between the PA and KA is localized along a deep-seated crustal ramp, probably close to the structural and metamorphic interface. The rocks of the PA may have acted as a rigid buttress against which the rocks of the KA piled up during Cordilleran crustal thickening.

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)0.001
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 score0.015
Threshold uncertainty score0.110

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0030.004
Science and technology studies0.0020.001
Scholarly communication0.0020.000
Open science0.0010.001
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 head0.006
GPT teacher head0.178
Teacher spread0.172 · 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".

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Citations0
Published2020
Admission routes1
Has abstractyes

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