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Record W2343749774 · doi:10.14288/1.0053529

Geology of the Topley intrusives in the Endako area British Columbia

2012· article· en· W2343749774 on OpenAlexaboutno aff
Edward Gordon Bright

Bibliographic record

VenuecIRcle (University of British Columbia) · 2012
Typearticle
Languageen
FieldSocial Sciences
TopicArchaeology and Natural History
Canadian institutionsnot available
Fundersnot available
KeywordsGeologyArchaeologyOceanographyGeography

Abstract

fetched live from OpenAlex

Granitic rocks of the Topley intrusives underlying 100 square miles, centered around Endako, north central British Columbia, form part of a composite body which lies in a northwest trending belt of granitic plutons extending from Babine Lake to Quesnel, a distance of 180 miles. Rocks of the Topley complex in the Endako area have intruded volcanic rocks of the Takla Group (Upper Triassic to Jurassic) and are unconformably overlain by flat-lying Tertiary volcanic flows. These intrusions are probably of Lower Jurassic to Lower Cretaceous age. The granitic rocks, ranging from diorite to alaskite form six large separately emplaced and sharply bounded intrusive bodies. The development of the Topley complex can be divided chronologically, from oldest to youngest, into five major stages: (I) the Simon Bay (diorite) complex; (II) the Endako quartz monzonite which is the host rock of the Endako molybdenum deposit, and the Franco is granite; (III) the Glennanan complex; (IV) the Casey quartz monzonite-alaskite; and (V) the Stellako quartz monzonite. The Glennanan complex, which is the best exposed and most intensely studied intrusive, consists of two large asymmetrically zoned bodies and a small stock of porphyritic quartz monzonite. The larger zoned body near the town of Endako has: (1) a western zone of porphyritic granite; (2) an intermediate zone of porphyritic quartz monzonite; and (3) an eastern zone of porphyritic granodiorite. A granodiorite zone is absent in the asymmetrically zoned Nithi Mountain intrusive body. All internal contact are gradational and all rock zones contain large rectangular perthite megacrysts which enclose oriented crystals of plagioclase and other minerals. The development of the rock zones can be accounted for by differentiation of a hornblende-biotite granodiorite magma at depth and successive intrusion of first granite, then quartz monzonite and finally granodiorite. Topley stages II to V represent a continuous period of epizonal intrusion following the emplacement of the more deep seated (mesozonal?) Simon Bay complex. Northwesterly and northeasterly trending fracture zones controlled the structural evolution of the Topley complex in the map area.

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)0.001
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesScience and technology studies
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.200
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0010.003
Scholarly communication0.0000.000
Open science0.0010.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

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 head0.010
GPT teacher head0.195
Teacher spread0.185 · 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.

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
Published2012
Admission routes1
Has abstractyes

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