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Record W2981666583 · doi:10.4095/289889

Geology and mineralization of the link between Hope Bay and Elu Greenstone Belts, northeastern Slave Craton, Nunavut

2012· report· en· W2981666583 on OpenAlexaffabout
Hubert Mvondo, D Lentz, Marc Bardoux, D T James

Bibliographic record

Venuenot available
Typereport
Languageen
FieldEarth and Planetary Sciences
TopicGeological Studies and Exploration
Canadian institutionsNatural Resources Canada
Fundersnot available
KeywordsBayGeologyGreenstone beltCratonMineralization (soil science)GeochemistryArcheanOceanographyPaleontologyTectonics

Abstract

fetched live from OpenAlex

Located in the NE Bathurst Block of the Slave Craton, the Hope Bay and Elu belts are two Neoarchean greenstone belts striking N-S and NE-SW, respectively. The Elu Belt (EB) southern end is deflected westwards to form a concave connection termed the Elu Link (EL) where 2716 to 2663 Ma supracrustals are in part shared with the adjacent Hope Bay Belt (HBB). The EL supracrustal sequence consists mainly of tholeiitic pillowed metabasalts with lesser amounts of interleaved metadacite, metarhyolite, iron formation, and metashale, having variably recorded D1 - D3 deformation. Supracrustals appear to be seamlessly in contact with syn-D1 migmatite orthogneiss on the EL eastern margin. Orthogneiss and supracrustal rocks were both intruded by syn- to late-D2 metagabbros and metagranites. Like in the HBB, Archean magmatic rocks of the EL originated from deep and upper mantle sources in a probable back-arc setting. Sparse NE-striking Proterozoic dolerite dikes derived from deep mantle sources cut the entire rock mass. D1 deformation was successively accompanied by hydrothermal alteration and prograde metamorphism reaching epidote-amphibolite facies peak conditions, but related structures are strongly obscured by D2 + D3 overprint. D2 that initiated under prograde metamorphism and was further accompanied by greenschist retrogression deformed D1 fabrics around tight to open curvilinear F2 folds forming a foliation triple junction between the EB + HBB. The F2 folds together with L2 radial stretching lineation and coeval shear zones show that the EL is rimmed around a syn-compression large-scale D2 dome. D3 is a brittle-ductile deformation lacking any visible fabric. Both D2 + D3 denote vertical general flattening dominated transpression with E-W maximum compression and N-S minimum extension. They illustrate asymmetric syn-compression exhumation of the HBB and EB that were further affected by strain-free greenschist retrogression due to the Thelon Orogeny. The mineralization comprising Au-As-Cu-Zn metals in most EL rock units occurred prior and, possibly, during metamorphism, was further remobilized by subsequent tectonic and thermal events. It follows that ore mineralization occurrence in the EL is chiefly lithologically and structurally controlled.

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)0.000
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 score0.320
Threshold uncertainty score0.644

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.001
Science and technology studies0.0010.001
Scholarly communication0.0010.000
Open science0.0000.001
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 head0.046
GPT teacher head0.233
Teacher spread0.187 · 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
Published2012
Admission routes2
Has abstractyes

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