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Record W25253324 · doi:10.7748/nm.21.6.17.s22

Insights Into Middle Crustal Processes In Magmatic Arcs, Coast Mountains, British Columbia

2009· dissertation· en· W25253324 on OpenAlexaboutno aff
Gabriela V. Depine

Bibliographic record

Venuenot available
Typedissertation
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsnot available
Fundersnot available
KeywordsGeologySeismologyEarth scienceGeochemistryArchaeologyGeography

Abstract

fetched live from OpenAlex

This thesis explores processes occurring in the middle and lower crust of magmatic arc-settings. This study is based on observations on the Coast Mountains of British Columbia, Canada, at ~53 degree N latitude. The rocks exposed at the surface in this area represent the roots of a Mesozoic to early Tertiary magmatic arc. Transpressional deformation occurred synchronously with magmatism and metamorphism from the Late Cretaceous to the Early Eocene. Between 61 and 50 Ma, the entire Canadian Cordillera tracks a period of extension and exhumation of high-grade metamorphic rocks, synchronous with intensified magmatism. The thermal state of the crust during this time period was explored using numerical models. The models attempt to reproduce a geotherm that explains observations found in the field, such as abundance of amphibolitic migmatites, widespread magmatism, granulite facies metamorphism, and high-temperature low-pressure metamorphism. The resulting geotherm is isothermal from the pluton emplacement depth to the Moho. The temperature of the profile is buffered by the solidus temperature of the country-rock. The upper crust is characterized by a steep temperature gradient of ~50 degree C/km. The structure and petrology of three plutons was analyzed to better understand pluton emplacement processes. Two of the plutons, the Kitlope and Quottoon plutons; are characterized by steep foliations and intruded during transpression. The third pluton, the Chief Matthew's pluton; intruded as a sub-horizontal sill during extension. The transposition of the foliation from vertical to horizontal is explained by the development of melt-filled tension gashes oriented perpendicular to the sub-vertical foliation. Melt migration results in melt accumulation in the gashes. This process coupled with a change from regional transtension caused development of flat foliation localized around the Chief Mathew's pluton. The exhumation path and cooling history of the three plutons was also explored. Petrology, geothermobarometry, geochemistry, and cooling ages were analyzed to determine that: 1) exhumation of ~6 km of rock occurred between the emplacement of the Quottoon and Chief Matthew's plutons at a rate of ~2-3 mm/yr; 2) the rocks cooled at a rate of ~50 degree C/Ma; 3) the area cooled below the biotite closure temperature by 51 Ma. An exhumation model integrating the studied area with the rest of the Canadian Cordillera is also proposed.

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 score0.106

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.004
Science and technology studies0.0030.001
Scholarly communication0.0020.001
Open science0.0010.001
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0100.001

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 head0.008
GPT teacher head0.190
Teacher spread0.182 · 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

Citations0
Published2009
Admission routes1
Has abstractyes

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