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Record W3109906647

Deformation history and gold mineralization of the Cadillac Group north of the Larder Lake-Cadillac deformation zone, southern Abitibi greenstone belt, Quebec

2019· dissertation· en· W3109906647 on OpenAlexfundaboutno aff
B. Samson

Bibliographic record

VenueLu Zone Ul (Laurentian University) · 2019
Typedissertation
Languageen
FieldComputer Science
TopicGeochemistry and Geologic Mapping
Canadian institutionsnot available
FundersUniversity of Toronto
KeywordsGreenstone beltGeologyDeformation (meteorology)Group (periodic table)Mineralization (soil science)GeochemistryArcheanOceanography
DOInot available

Abstract

fetched live from OpenAlex

The Cadillac Group is located immediately north of the Larder Lake–Cadillac deformation zone (LLCDZ) along the southern margin of the Abitibi greenstone belt in the Archean Superior Province, Quebec. The LLCDZ is a major 250 km long structure known for hosting several gold deposits. It is generally east-trending over a distance of 170 km, and then it swings to the southeast over a distance of 35 km along the so-called Malartic segment, before resuming its easterly trend for another 45 km. With its thick sequence of <2687 Ma turbiditic sandstone interlayered with mudstone and polymictic conglomerate, the Cadillac Group provides favourable rocks for studying the structural history of the Malartic segment which, due to its unique trend, is important for understanding the overall tectonic evolution of the LLCDZ. Deformation of the Cadillac Group began with large-scale isoclinal folding and the formation of a regional cleavage parallel to the trend of the Malartic segment (D1 event). These structures overprint a 2675.5 ± 2 Ma quartzfeldspar-phyric (QFP) intrusion providing a maximum age for the D1 event and a minimum age for the deposition of the Cadillac sequence. The deformation of the Cadillac Group resumed with bedding-parallel sinistral shearing and the emplacement of gold-bearing extensional quartz veins (D2 event), and continued with bedding-parallel dextral shearing, Z-shaped folding, the formation of a cleavage oriented oblique (anticlockwise) to the trend of the Malartic segment, and by the rotation and segmentation of the gold-bearing veins (D3 event). Contrary to previous interpretations of the Malartic segment as an early pre-D1 accretionary structure, it is interpreted as the short limb of a broad Z-shaped flexure that formed during D3 folding of the LLCDZ and that postdates the emplacement of gold-bearing veins in the Cadillac Group. Mineralized veins at the nearby worldclass Canadian Malartic deposit were emplaced during the same D2 event but they differ in alteration mineralogy and geochemistry to the Cadillac veins suggesting different sources for the mineralizing fluids. Mineralization at the Lapa deposit is similar in sulphide mineralogy and metal association to the Cadillac veins but was emplaced earlier during the deformation history of the LLCDZ.

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 score0.989
Threshold uncertainty score0.146

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 science0.0010.001
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0050.000

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 head0.006
GPT teacher head0.159
Teacher spread0.153 · 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
Published2019
Admission routes2
Has abstractyes

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