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Record W2336776009 · doi:10.14288/1.0167211

The petrology and petrogenesis of the Ren carbonatite sill and fenites, southeastern British Columbia, Canada

2014· article· en· W2336776009 on OpenAlexaffabout
Avee Ya’acoby

Bibliographic record

VenueOpen Collections · 2014
Typearticle
Languageen
FieldEngineering
TopicHydrocarbon exploration and reservoir analysis
Canadian institutionsUniversity of British Columbia
Fundersnot available
KeywordsPetrogenesisGeologyCarbonatiteSillPetrologyArchaeologyGeochemistryGeographyBasalt

Abstract

fetched live from OpenAlex

This thesis explores in detail the petrology and petrogenesis of the Ren carbonatite sill and associated fenites, located in the Monashee mountain range of British Columbia. The carbonatite body and fenites have been significantly deformed and metamorphosed, which has provided a unique petrological research opportunity, since only a few other carbonatite occurrences worldwide have been described from highly metamorphosed orogenic settings. This work aims to address knowledge gaps pertaining to the petrology, petrogenesis and economic exploration of comparable carbonatites in similar geotectonic settings. The effects of amphibolite facies regional metamorphism and progressive deformation are apparent throughout the carbonatite body and adjacent fenites. Many of the rocks display remobilized, passively mixed components, boudinaged structures, and rheomorphic bands, as well as foliation and porphyroblastic textures. Recrystallization of minerals at peak metamorphic conditions (580–730 °C) is indicated primarily in undifferentiated calcite for which metamorphic solvus temperatures (~690 °C) were derived. Other minerals related to metamorphic recrystallization include rims of monazite-(Ce) around earlier fluorapatite, interstitial REE-silicates, and Ca- and Mg-amphibole forming late in the paragenetic sequence, after primary silicates. Despite the metamorphic overprint and alteration, many petrological features pertaining to the igneous paragenetic record have been preserved, such as textures of primary minerals, compositional trends in phlogopite, clinopyroxene and amphibole, and whole-rock geochemistry of rock units. Solvus temperatures (~760 °C) of calcite, higher than peak metamorphic conditions, highlight preservation of the igneous component. The carbonatite is inferred to be a product of primitive mantle melts(s) that did not undergo significant fractionation processes, and intruded the crustal environment relatively undifferentiated. The whole-rock compositional trend of the fenites and partially fenitized host rocks suggests sodic-potassic alteration of the country rock during emplacement of the carbonatite sill. The Nb-Ta and REE mineralizations of the Ren occurrence are both insufficient for economic extraction. Nevertheless, rare and new mineral candidates, (Fe,OH)-analogue to västmanlandite-(Ce) and (Mg)-analogue to biraite-(Ce), discovered in the deposit by the author, emphasize its petrological and mineralogical significance.

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: Not applicable · Consensus signal: Not applicable
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.336
Threshold uncertainty score0.828

Codex and Gemma teacher scores by category

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

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 head0.004
GPT teacher head0.166
Teacher spread0.162 · 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 designNot applicable
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
Published2014
Admission routes2
Has abstractyes

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