MétaCan
Menu
← Back to cohort
Record W1726060625 · doi:10.20381/ruor-12811

Geology, structure and gold mineralization within the Porcupine-Destor Deformation Zone, Harker-Holloway gold camp, southwestern Abitibi Greenstone Belt, Canada

2004· dissertation· en· W1726060625 on OpenAlexaboutno aff
Brian Richard Luinstra

Bibliographic record

VenueuO Research (University of Ottawa) · 2004
Typedissertation
Languageen
FieldComputer Science
TopicGeochemistry and Geologic Mapping
Canadian institutionsnot available
Fundersnot available
KeywordsGreenstone beltGeologyArcheanMineralization (soil science)GeochemistryGeomorphology

Abstract

fetched live from OpenAlex

The Harker-Holloway gold camp is located along the Porcupine-Destor Deformation Zone in the northern portions of Harker and Holloway Townships, Ontario. The gold camp is host to two operating gold mines, the Holloway and Holt-McDermott mines as well as several minor gold showings. The Holloway and Holt-McDermott deposits are located entirely within splays of the Porcupine-Destor Deformation Zones within meta-volcanic rocks of the Kidd-Munro and Kinojevis lithotectonic assemblages, respectively, and are separated by a narrow band of Timiskaming meta-sedimentary rocks. The rocks of the area form a steeply south dipping package within which rocks have been deformed associated with development of the Porcupine-Destor Deformation Zone. Within the Holloway mine, a polylithic breccia folded into the volcanic stratigraphy was dated at 2686.6 +/- 1.8 Ma. Meta-volcanic rocks which host the two deposits belong to a tholeiitic suite of rocks and can be separated into four distinct groups based on lithogeochemistry. Tholeiites all have flat lying REE profiles and can be grouped into Types I, II and III based on increasing normalized REE values and are interpreted to represent a fractional crystallization trend from a tholeiitic source magma. An additional trachytic meta-volcanic unit was identified in the Holt-McDermott mine and is characterized by an enriched LREE profile and is interpreted to have formed via fractional crystallization from tholeiitic magma. Several episodes of gold mineralization have been identified in the area. The first and most economically important gold mineralizing event (Au1) is associated with albite alteration (Ab) and pyrite mineralization (Py1). Primary gold mineralization (Au1) predates D1 deformation, and is confined to specific stratigraphic units bounded by zones of intense S1 foliation development. A second, volumetrically less important, gold mineralization (Au2) is located within haloes of subhorizontal quartz-carbonate veins which cross cut the S1 foliation. Secondary mineralization is associated with a sericite+carbonate alteration (Sr) and a second generation of pyrite mineralization (Py2) and is interpreted to be a remobilization of primary gold mineralization. A third, volumetrically minor, gold mineralization event (Au3) is associated with N to NNE striking quartz veins which cross cut all other structures. (Abstract shortened by UMI.)

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 score0.013
Threshold uncertainty score0.094

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.003
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 head0.015
GPT teacher head0.231
Teacher spread0.216 · 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
Published2004
Admission routes1
Has abstractyes

Explore more

Same venueuO Research (University of Ottawa)→Same topicGeochemistry and Geologic Mapping→French-language works237,207→