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Record W3154473443

Metallogeny and characterization of late cretaceous superimposed porphyry Cu-Au-Mo and epithermal Au-Ag systems in the Dawson Range, Yukon, Canada: case study on the Klaza deposit

2021· dissertation· en· W3154473443 on OpenAlexaboutno aff
Well-Shen Lee

Bibliographic record

VenueLu Zone Ul (Laurentian University) · 2021
Typedissertation
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsnot available
Fundersnot available
KeywordsMetallogenyGeologyCretaceousGeochemistryRange (aeronautics)Characterization (materials science)PaleontologyEngineeringMaterials sciencePyrite
DOInot available

Abstract

fetched live from OpenAlex

The Dawson Range Gold Belt (DRGB; Yukon’s richest mineral district by resource) lies
\nin the Yukon segment of the North American Cordillera and is dominated by Late Cretaceous
\n(77–74 Ma) porphyry-epithermal systems. Mineral occurrences in the DRGB have seen limited
\nexploration due to: (1) poor surface exposure; (2) incoherent classification of intrusive rocks; and
\n(3) outdated exploration models.
\nA multidisciplinary study utilizing: (1) field observations (drill core logging and
\nmapping); (2) geochronology (U-Pb in zircon by LA-ICP-MS and CA-TIMS; Ar-Ar in
\nmuscovite; Re-Os in molybdenite); (3) whole-rock geochemistry; (4) zircon trace element
\ngeochemistry; (5) petrography (SEM-EDS, optical microscopy); and sulfide mineral
\ngeochemistry (LA-ICP-MS element maps) is designed to address the above challenges through a
\ndetailed investigation on the well-preserved Klaza deposit using 2011-2020 drilling data.
\nResults suggest the presence of six intrusive phases of mafic to intermediate
\ncompositions. Intrusive activity occurs in four pulses spanning the Late Triassic to the Late
\nCretaceous. The Late Cretaceous magmatic pulse is protracted (80–65 Ma) and displays timedependant compositional changes. The youngest plutonic suites: (1) display enrichments in
\nLREEs relative to the older suites; (2) are related to garnet-bearing sources (depleted HREEs,
\nhigh La/Yb); (3) are hydrous (presence of hornblende-biotite); and (4) reflect a dynamic magma
\nchamber (magma mixing textures).
\nTwo clusters of hydrothermal ages are constrained (ca. 77 Ma and ca. 71 Ma), correlating
\nwith Casino suite and Prospector Mt. suite magmatism, respectively. Higher temperature A-, B-and EDM-like veins are related to the 77 Ma event and cut by fault-veins related to the 71 Ma
\nevent. The fault-veins consist of four stages. Gold is hosted in early (Stage 2a, 2b) arsenopyrite
\nand pyrite lattices and later liberated through late (Stage 2d) Copper-bearing fluids, whereas
\nsilver occurs later (Stage 2c) as native silver and sulfosalts.
\nThe Klaza system is best described as a porphyry-related intermediate sulfidation
\nepithermal deposit superimposed on an older, unrelated porphyry system. Similar observations of
\nspatial-temporal overprinting are documented throughout the DRGB (e.g., Casino deposit and
\nFreegold Mt. district), suggesting these Late Cretaceous porphyry systems are linked to a fertile
\nmetallogenic event spanning 15 million years. This study is the first detailed characterization of
\nLate Cretaceous porphyry systems in the DRGB and presents the first use of machine learning assisted paragenetic study of sulfide minerals for exploration and improving ore body
\nknowledge.

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)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation 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 score0.216
Threshold uncertainty score0.597

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0000.000

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 head0.009
GPT teacher head0.169
Teacher spread0.160 · 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.

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

Citations1
Published2021
Admission routes1
Has abstractyes

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