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Record W2186130837

STRATIGRAPHIC IMPLICATIONS FOR MINERALIZATION: PRELIMINARY FINDINGS OF A METALLOGENIC INVESTIGATION OF THE TALLY POND VOLCANICS, CENTRAL NEWFOUNDLAND

2003· article· en· W2186130837 on OpenAlexaboutno aff
Paul J. Moore

Bibliographic record

Venuenot available
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeological and Geochemical Analysis
Canadian institutionsnot available
Fundersnot available
KeywordsGeologyRhyoliteFelsicVolcanic rockGeochemistryMaficUnconformityVolcanoSilicicPyroclastic rockSedimentary rock
DOInot available

Abstract

fetched live from OpenAlex

Preliminary investigation of volcanogenic massive sulphide occurrences within the Tally Pond volcanics, suggests mineralization is intimately associated with a sequence of quartz-phyric , high-silica rhyolite flows and epiclastic sedimentary rocks. These mineralized rocks are hosted within a bimodal volcanic pile, where correlation as a single magmatic event cannot be confirmed but the available age-date determinations suggests the correlation of at least one widespread mineralizing event. This is demonstrated by identical U–Pb (zircon) dates (513 ± 2 Ma) obtained by previous workers, from similar quartzphyric volcanic rocks from the Duck Pond–Boundary deposit area and the Lemarchant prospect. Based mainly on observations of drill core from the Duck Pond and Boundary deposits, the internal stratigraphy of the Tally Pond volcanics appears to attest to a prolonged period of mafic volcanism, punctuated by several felsic volcanic episodes. The oldest felsic volcanic event is recorded as a thick sequence of flow-dominated aphyric to feldspar-phyric dacitic to rhyolitic volcanic rocks having textures indicative of a lobe-hyaloclastite flow volcanic regime. This sequence is con formably overlain and possibly locally intercalated, with an apparently less voluminous sequence of high-silica, quartzphyric, rhyolite and epiclastic turbidites that host, and is chronologically and perhaps genetically, linked with volcanogenic massive sulphide mineralization. Based on a review of available geochemical, geochronological and isotopic data, the Tally Pond volcanics are interpreted to have formed in an ensimatic-arc environment, as originally proposed by previous workers. However, it is further pro posed that this arc formed adjacent to the Gondwanan continental margin as evidenced by characteristic highly radiogenic Pb-isotopic signatures, observed from massive sulphides within the Tally Pond volcanics and the Victoria Lake supergroup. Tectono-magmatic models, proposed for pre- and post-Arenig volcanic rocks of similar tectonic affinities, within the Wild Bight and Exploits groups elsewhere in the Exploits Subzone, may apply to arc-related volcanic rocks of the Victoria Lake supergroup, including the Tally Pond volcanics, suggesting further links between these two metallogenically important areas.

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 score0.324
Threshold uncertainty score0.651

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 science0.0000.001
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 head0.017
GPT teacher head0.200
Teacher spread0.183 · 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

Citations9
Published2003
Admission routes1
Has abstractyes

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