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Record W3041747834

A paleomagnetic study of ca. 580 Ma volcanics near Grand Bank, Avalon zone of Newfoundland, and implications for true polar wander in the ediacaran

2018· dissertation· en· W3041747834 on OpenAlexaboutno aff
J. P. Hodych

Bibliographic record

VenueMemorial University Research Repository (Memorial University) · 2018
Typedissertation
Languageen
FieldEarth and Planetary Sciences
TopicPaleontology and Stratigraphy of Fossils
Canadian institutionsnot available
Fundersnot available
KeywordsPaleomagnetismGeologyApparent polar wanderLaurentiaVolcanic rockPaleontologyRemanenceTephraGeophysicsSeismologyVolcanoPaleozoicMagnetic fieldPhysics
DOInot available

Abstract

fetched live from OpenAlex

Paleomagnetic studies suggest that Laurentia moved from the equator to the pole and then back \nagain within ~60 Ma during the Ediacaran. Hypotheses to explain the large 90⁰ apparent oscillations \ninclude unreliable paleomagnetic data and/or unreliable dating and complex magnetic \nfield behaviour. Inertial interchange true polar wander (IITPW) has also been suggested. Since \nIITPW would be a global event, it would require the large oscillations suggested by the paleomagnetic \nrecord of Laurentia to have affected all the continents in the Ediacaran. Such oscillations \nhave been found in selected paleomagnetic data from Baltica and West Africa but not Australia. \nAvalonia paleomagnetism also does not appear to show the oscillations expected from the IITPW \nhypothesis. The present study provides new paleomagnetic data for the Marystown Group volcanics, \ndated at 580±3 Ma, collected near Grand Bank in the Avalon Zone of Newfoundland. \nThe volcanics were studied with alternating field and thermal demagnetization which showed that \nremanence is carried mostly by magnetite rather than hematite. Seven sites provide stable remanence \ndirections with mean tilt-corrected declination and inclination of D=287⁰ and I=58⁰ (α95 = \n13.7⁰). A positive conglomerate test, using rhyolitic crystal lithic tuff clasts from an agglomerate \nwithin the section of flows, shows that the magnetite-bearing clasts carry primary remanence. \nMagnetic polarity reversals are also present within the section (six normal flows and one reversed \nflow). The corresponding paleolatitude is 39⁰+17/-13⁰ at 580±3 Ma. This agrees with the paleolatitude \nof 35⁰+11/-10⁰ at 580±10 Ma previously found for three basalt flows and five red bed sites \nin the Marystown Group (omitting the likely Devonian Famine Back Cove basalts). The Marystown \nGroup results, along with other stable paleomagnetic data from Avalonia, suggest that Avalonia \nremained at mid to low latitudes during the mid-Ediacaran. The declination of Avalonia suggests \nthat it remained at 225⁰ from 606 Ma to 592 Ma and then underwent a steady change towards \n330⁰ at 550 Ma. Although IITPW cannot be disproved for the mid-Ediacaran, it is more likely \nthat complex magnetic field behaviour is the reason multiple large oscillations can be seen in the Laurentia, Baltica, and West African Craton paleomagnetic data.

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 score0.173
Threshold uncertainty score0.349

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 science0.0000.000
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 head0.025
GPT teacher head0.261
Teacher spread0.236 · 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
Published2018
Admission routes1
Has abstractyes

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