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Record W7014464543

Petrogenesis and Metallogenesis of the Ultramafic Layered North Lac Des Iles Intrusion in the Lac Des Iles Complex, Ontario, Canada

2017· dissertation· en· W7014464543 on OpenAlexfundaboutno aff

Bibliographic record

VenueQSpace (Queen's University Library) · 2017
Typedissertation
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsnot available
FundersQueen's University
KeywordsLayered intrusionMineralization (soil science)Ultramafic rockLiquationSulfideIntrusion
DOInot available

Abstract

fetched live from OpenAlex

A detailed petrologic and metallogenic study was conducted on the eastern flank of the Northern Ultramafic Centre (NUC) of the North Lac des Iles Complex (North LDIC) to understand the petrogenesis of cyclically layered ultramafic cumulates and the processes involved in the formation of the PGE mineralization. Additional investigation of historical PGE-Cu-Ni prospects in the North LDIC provides insights into the styles of mineralization and how these styles compare with the stratiform PGE mineralization of the NUC and the Pd deposits hosted by the mafic Mine Block Intrusion of the South Lac des Iles Complex (South LDIC). Field relationships, mineralogical, textural, mineral chemical, and lithochemical data from the NUC reveal the presence of two distinct paragenetic sequences of cumulate rocks. Cyclic Unit A (CUA) is characterized by an upward progression of Ol+Cr-SpOl+Opx+Cpx±Cr-SpCpx+Opx Pl+Opx±Cpx. Cyclic Unit B (CUB) exhibits a cumulate stratigraphic progression of Ol+Cr-SpOl+Cpx. CUA sequences are interpreted to have formed by fractional crystallization of more siliceous ultramafic magmas relative to CUB parent magmas. Stratiform PGE mineralization of the Sutcliffe Zone is typically hosted within four different CUA units. PGE mineralization is commonly associated with >2% disseminated Cu-Ni sulfide, and is characterized by mantle-like S/Se ratios, Pd tenors in sulfide <1000 ppm, and Pd/Pt ratios < 5. The Sutcliffe Zone is interpreted to have formed by a combination of fractional crystallization and dynamic recharge and mixing of CUA and CUB parental magmas. The majority of PGE-Cu-Ni prospects in the North LDIC share similar host rocks, sulfide and platinum group mineral compositions and textures, trace element signatures, Pd tenors, S/Se and Pd/Pt ratios as the stratiform PGE mineralization at Sutcliffe Zone, similar genesis. Similarities between stratiform PGE-Cu-Ni mineralization in the North LDIC and the magmatic breccia-style Pd mineralization in the South LDIC include the prevalence of orthopyroxene, widespread magmatic alteration, low sulfide content, Pd-rich PGE mineralization and the dominance of Pd-bismuthotellurides. Despite these similarities, the two styles of mineralization remain distinct in terms of structural controls on mineralization, host rocks, base metal sulfide and PGE mineralogy, PGE tenors of sulfide, and the source of parental magmas.

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 score0.024
Threshold uncertainty score0.176

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.002
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 head0.011
GPT teacher head0.162
Teacher spread0.152 · 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
Published2017
Admission routes2
Has abstractyes

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