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Record W4237125776 · doi:10.22215/etd/2013-09977

Structural, Geochronological, and Thermochronological Constraints on the Evolution of Orogenic Infrastructure in the Thor-Odin – Pinnacles Area of Southeastern British Columbia.

2013· dissertation· en· W4237125776 on OpenAlexaboutno aff
Deanne van Rooyen

Bibliographic record

Venuenot available
Typedissertation
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsnot available
Fundersnot available
KeywordsGeologyThermochronologyZirconBasementGeochronologyGneissMetamorphismTerraneDome (geology)GeochemistryMetamorphic rockProterozoicPetrographyCrustPaleontologyTectonicsArchaeology

Abstract

fetched live from OpenAlex

The Thor-Odin dome is a basement-cored tectonothermal culmination in the southeastern Canadian Cordillera containing high grade metamorphic rocks, tectonically overlain by a heterogeneous tract of polydeformed medium to high grade metamorphic rocks exposed in the footwall of the Columbia River fault system. The Thor-Odin and Frenchman Cap domes comprise Paleoproterozoic “basement” gneiss infolded with Proterozoic to Paleozoic metasedimentary “cover” rocks. Detrital zircon geochronology from three samples of the inferred basal quartzite within the Thor-Odin dome contain two separate maximum depositional age populations at <1.65 Ga and <1.1 Ga, suggesting two temporally separate quartzite units, neither of which is correlative with the basal quartzite in the Frenchman Cap dome, c. 1.85 Ga. A Neoproterozoic to Cambrian panel structurally overlies the dome, as evidenced by a <600 Ma quartzite on Mount Symonds. Middle Jurassic, or younger, quartzites are present at Plant Creek, representing a transposed terrane boundary and the accretion of rocks on to the Laurentian margin. Four tectonothermal domains were defined based on timing of metamorphism, deformation and cooling, structural and petrographic data, and 40Ar/39Ar thermochronology. The structurally highest domain (Whatshan – Pinnacles) was polyfolded in the Late Cretaceous. The second highest domain (South Fosthall) was penetratively deformed in the mid-crust at c. 73 – 64 Ma. Deformation ended in the rocks of the South Fosthall area after c. 64 Ma, but continued in the structurally lower third domain (North Fosthall – Cariboo Alp). The North Fosthall– Cariboo Alp domain became suprastructure relative to the deforming rocks in the structurally lowest domain (Thor-Odin dome) after c. 58 Ma. The Thor-Odin dome remained in the infrastructure until c. 52 Ma. Exhumation and cooling through 500 ⁰C in the upper part of the structural section was ongoing during the last stages of transposition and folding in the dome in the Late Paleocene to Early Eocene. All the rocks cooled through 300 ⁰C together between 52.5 – 51 Ma. Extensional structures were active at all structural levels by c. 51 Ma, reflecting a regional switch from transpression to transtension, expressed as crustal scale extension and exhumation via the east-dipping Columbia River and west-dipping Okanagan Valley extensional fault systems.

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 score0.029
Threshold uncertainty score0.067

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.002
Science and technology studies0.0010.001
Scholarly communication0.0010.000
Open science0.0010.001
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0020.000

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 head0.011
GPT teacher head0.192
Teacher spread0.181 · 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

Citations2
Published2013
Admission routes1
Has abstractyes

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