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Record W1539203024 · doi:10.1029/2007tc002103

Timescales of migmatization, melt crystallization, and cooling in a Cordilleran gneiss dome: Valhalla complex, southeastern British Columbia

2008· article· en· W1539203024 on OpenAlexaboutno aff
Stacia M. Gordon, Donna L. Whitney, Christian Teyssier, Marty Grove, W. J. Dunlap

Bibliographic record

VenueTectonics · 2008
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsnot available
Fundersnot available
KeywordsGeologyZirconGeochemistryMonaziteGneissMigmatiteThermochronologyMetamorphismGeochronologyPartial meltingTitaniteHornblendeBiotiteMetamorphic rockCrustPaleontology

Abstract

fetched live from OpenAlex

Integration of in situ and conventional ion microprobe U‐Th‐Pb zircon and monazite geochronology with 40Ar/39Ar hornblende, biotite, and muscovite thermochronology provides a temporal record of metamorphism, partial melting, fluids, and cooling of exhumed midcrustal to lower crustal rocks. The Valhalla complex, southeastern British Columbia, is one of a series of elongate gneiss domes within the Omineca belt of the Canadian Cordillera. We have performed U‐Th‐Pb and 40Ar/39Ar age measurements on migmatitic gneisses from a range of structural levels and settings within the Valhalla complex in an effort to better document the timing of migmatization and exhumation. Stromatic migmatites and leucosomes crystallized in boudin necks yield concordant U‐Pb zircon ages that cluster near 60 Ma and Th‐Pb monazite ages of circa 60–50 Ma. In situ analyses of monazite in samples that contain <10% leucosome yield a bimodal distribution at 70–65 and 62–57 Ma. The younger ages are similar to migmatite zircon ages. 40Ar/39Ar analyses from the same rocks document cooling at 51–49 Ma. These new data, combined with field, structural, and petrologic data from this and previous studies of the Omineca domes, indicate that a large region (thousands of km2) of orogenic crust may have been partially molten during the Early Tertiary (>60–50 Ma). However, the combined data also suggest that melt crystallization (circa 60 Ma) in the Valhalla complex occurred rapidly and before the other domes within the Omineca belt. Cooling at 49 Ma throughout the Omineca is associated with regional extension and exhumation of migmatites in the domes. The presence of abundant migmatites and the similarity in timing of melt crystallization and cooling in domes along the 400‐km‐long Omineca belt is consistent with localization of exhumation at the boundary between the flowing crust of the hinterland and the rigid, colder crust of the Rocky Mountain foreland.

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 score0.026
Threshold uncertainty score0.099

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 studies0.0020.001
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 head0.015
GPT teacher head0.187
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".

Quick stats

Citations80
Published2008
Admission routes1
Has abstractyes

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