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Record W4406596058 · doi:10.1016/j.gr.2025.01.007

Paleomagnetic consequence of thermal evolution of the North American Passive Margin: The Jurassic APWP controversy

2025· article· en· W4406596058 on OpenAlexafffund
Masoud Mirzaei, Russell F. Burmester, Bernard Housen, Vadim A. Kravchinsky

Bibliographic record

VenueGondwana Research · 2025
Typearticle
Languageen
FieldBiochemistry, Genetics and Molecular Biology
TopicGeomagnetism and Paleomagnetism Studies
Canadian institutionsUniversity of Alberta
FundersNatural Sciences and Engineering Research Council of Canada
KeywordsGeologyPaleomagnetismMargin (machine learning)PaleontologyPassive marginGeophysicsRiftTectonics

Abstract

fetched live from OpenAlex

• New hypothesis for North American paleomagnetic Jurassic data discord. • Updated and refined Triassic-Jurassic APWP for the North American craton. • Reassessment of eastern vs. southwestern Jurassic paleomagnetic data. • Post-rifting thermal flexure deviated eastern group results on NA passive margin. • Three phases revealed for NA passive margin evolution during Jurassic. This study revisits the long-standing controversy in selecting Jurassic paleomagnetic data to define the North American (NA) craton APWP. Data from igneous rocks in the eastern part of NA and select global data rotated into NA coordinates define a high-latitude path. In contrast, the data from mostly sedimentary rocks in the NA Southwest interior (southwestern group) describe a lower-latitude path. Analysis suggests that previous explanations, such as inclination error in the southwestern group, cannot fully explain the disparity, and raises concerns that some magnetization of the eastern group may be partially secondary or younger, and others do not average secular variation. We present a new hypothesis that attributes the discrepancy to the post-tilt magnetization of the eastern NA continental margin caused by thermally induced non-uniform relative vertical movements during the post breakup evolution of northeast NA. This is tested by comparing mid-Jurassic paleomagnetic data of the eastern group with the coeval directions calculated from an updated late Triassic-Early Cretaceous reference NA APWP, presented here defined using a select and refined set of paleomagnetic poles mostly from southwestern region. One resolution is that a) after the breakup of NA from Africa (∼190 Ma), the thermally uplifted oceanside of the margin started to subside, while the more in-land regions experienced uplift due to landward lateral heat propagation in the lithosphere; b) during ∼190–140 Ma, the differential vertical motion tilted the edge of the margin eastward, about a horizontal axis with ∼53.5° azimuth. This eastward tilting peaked at ∼175–165 Ma and gradually decreased until ∼145–140 Ma. During this phase, the eastern group igneous rocks were emplaced and magnetized in this tilted framework; c) after ∼140–110 Ma, subsidence dominated the entire region. However, higher subsidence rates in more in-land parts tilted the marginal part along with their magnetizations acquired in the eastward-tilted position back (westward) to their current attitudes.

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 categoriesScience and technology studies
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.631
Threshold uncertainty score1.000

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 studies0.0000.003
Scholarly communication0.0000.000
Open science0.0010.000
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 head0.012
GPT teacher head0.283
Teacher spread0.271 · 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.

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

Citations2
Published2025
Admission routes2
Has abstractyes

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