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Record W2296344778 · doi:10.14288/1.0052896

The timing and structural evolution of the Donlin Creek gold deposit, southwest Alaska

2009· article· en· W2296344778 on OpenAlexaff
Kenneth Daniel MacNeil

Bibliographic record

VenuecIRcle (University of British Columbia) · 2009
Typearticle
Languageen
FieldComputer Science
TopicGeochemistry and Geologic Mapping
Canadian institutionsUniversity of British Columbia
Fundersnot available
KeywordsGeologyArchaeologyGeochemistryGeography

Abstract

fetched live from OpenAlex

Lithologic and structural data from more than 220 structurally oriented diamond drill holes are used to delineate the subsurface geology, 3-D geometry and to constrain the structural evolution of the >30 million ounce Donlin Creek gold deposit. The geology of the Donlin Creek gold deposit is characterized by north-northeast – south-southwest shortening that produced structural fabrics similar to those formed in thin-skinned fold and thrust belts. This deformation consists of dominantly southwest dipping thrust faults, subordinate northeast dipping back thrusts, and associated thrust ramp anticlines in the Kuskokwim Group sedimentary rocks. The fold and thrust style deformation is locally overprinted by northeast trending, low amplitude open folds interpreted to be related to regional dextral strike-slip tectonics. Low displacement, north-northeast striking, steeply southeast dipping normal faults cut the thrust faults and both generations of folds. The normal faults, northeast trending folds, and older fold and thrust geometry are intruded by a porphyritic dyke and sill swarm. Bedding discordant intrusions are emplaced along the north-northeast striking, steeply southwest dipping normal faults. Bedding concordant intrusions are most common in the folded sedimentary rocks in the hanging walls of thrust faults. The intrusions are cut by tensional gold being quartz ± carbonate + sulphide veins, which represent the youngest structural fabric. The distribution of veins is dictated by the rheology of the host rocks. For example, the brittle intrusions are the best host to gold mineralization; however veins are also present in coarse grained sedimentary rocks. U-Pb and ⁴⁰Ar/³⁹Ar geochronology provide absolute ages for deposition of the Kuskokwim sediments (~ 88 Ma), emplacement of the felsic intrusions (~71 Ma) and timing of gold mineralization (~ 71 Ma). These data indicate approximately 14.9 million years between initial sedimentation, emplacement of intrusions, and precipitation of gold mineralization. Geochronology constrains the timing of fold and thrust style deformation, and overprinting north-northeast trending folds to between ~ 88 Ma and ~ 71 Ma. The available geologic and geochronologic data also indicates that intrusion of the post-kinematic Late Cretaceous

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 score0.092
Threshold uncertainty score0.183

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 studies0.0010.000
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 head0.006
GPT teacher head0.161
Teacher spread0.155 · 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
Published2009
Admission routes1
Has abstractyes

Explore more

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