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Record W11866677 · doi:10.1517/14656566.3.3.265

Paleomagnetism and Rock Magnetism of "SEDEX" Zn-Pb-Cu Ores in Black Shales in Australia and Yukon and of Fluorite Veins in Granite in Newfoundland.

2011· article· en· W11866677 on OpenAlexfundaboutno aff
Kazuo Kawasaki

Bibliographic record

VenueExpert Opinion on Pharmacotherapy · 2011
Typearticle
Languageen
FieldBiochemistry, Genetics and Molecular Biology
TopicGeomagnetism and Paleomagnetism Studies
Canadian institutionsnot available
FundersNatural Sciences and Engineering Research Council of CanadaUniversity of Windsor
KeywordsGeologyPaleomagnetismGeochemistryFluoriteRock magnetismPaleontology

Abstract

fetched live from OpenAlex

The paleomagnetic age dating technique is used to study the genesis of a fluorite and four "sedimentary exhalative (SEDEX)" deposits which are hard to date by conventional radiometric methods because they lack suitable minerals, which causes controversy about their ore genesis. Paleomagnetic analysis of 359 specimens from the Devonian St. Lawrence Granite and fluorite veins in Newfoundland shows that the granite and fluorite veins are coeval and retain a primary remanence carried by pyrrhotite and/or magnetite. The difference between the measured and expected paleopoles is attributed to postemplacement counterclockwise rotation of ~17░ of the area about a vertical axis during the Late Devonian Acadian Orogeny. Paleomagnetic analysis of 333 specimens from the Century Zn-Pb-Ag deposit in Australia isolates a stable characteristic remanent magnetization (ChRM) for ore sites only that resides mainly in single (SD) or pseudosingle domain (PSD) titanomagnetite and pyrrhotite. A positive fold test shows that the ores ChRM predates D2 deformation in the Mesoproterozoic Isan Orogeny. The paleomagnetic age of 1558▒4 Ma supports a late diagenetic replacement model for ore genesis. Paleomagnetic and rock magnetic analyses of 333 specimens from the Mount Isa Zn-Pb-Cu-Ag and George Fisher Zn-Pb-Ag deposits in Australia isolate a stable ChRM carried mainly by SD or PSD pyrrhotite and/or titanomagnetite. The negative fold test shows that the ChRM postdates the ~1510 Ma D3 deformation in the Isan Orogeny. Thus the ~1505 Ma paleomagnetic age provides a minimum age for the ores and an age for the greenschist metamorphism during the orogeny. Paleomagnetic and rock magnetic analyses of 339 specimens from six mineralized panels in the Howards Pass Zn-Pb deposits in Yukon isolate a stable ChRM that mainly resides in SD or PSD pyrrhotite and titanomagnetite. The paleopole falls on Middle Jurassic portion of the North American apparent polar wander path (APWP) or corrected APWP for the Intermontane terranes, giving ~170 Ma and ~162 Ma, respectively. The results indicate that the Selwyn Basin had undergone ~35░ clockwise rotation with ~10░ northward translation between Middle Jurassic and mid-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 score0.965
Threshold uncertainty score0.069

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 studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
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 head0.036
GPT teacher head0.309
Teacher spread0.273 · 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
Published2011
Admission routes2
Has abstractyes

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