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Magnetoclimatology of aeolian sediments

2001· article· en· W2102069820 on OpenAlexaff
Michael Evans

Bibliographic record

VenueGeophysical Journal International · 2001
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeology and Paleoclimatology Research
Canadian institutionsUniversity of Alberta
Fundersnot available
KeywordsGeologyLoessAeolian processesLoess plateauSortingPhysical geographyGlacial periodInterglacialPaleontologyChinaPlateau (mathematics)QuaternaryCzechGeomorphologyEarth scienceSoil scienceGeographyArchaeology

Abstract

fetched live from OpenAlex

Two models—which lead to signals of opposite sign—are currently at the forefront of magnetoclimatological debates. In the classic sites of the Chinese Loess Plateau, soil formation during interglacials leads to magnetic enhancement in the palaeosols. In other regions (Alaska, Siberia), magnetic susceptibility peaks during glacial intervals. By looking at the broader picture, the relationship between these two models can be clarified. A simple qualitative analysis based on density sorting then determines the regimes under which one or the other dominates. Published data from Siberia, China, the Czech Republic and elsewhere permit a certain degree of quantification, and lead to the conclusion that proximal sites are likely to manifest Alaskan/Siberian‐type magnetoclimatological patterns. Beyond a few hundred kilometres, however, distal sites will be dominated by Chinese‐type patterns.

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 categoriesInsufficient payload (model declined to judge)
Consensus categoriesInsufficient payload (model declined to judge)
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.042
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
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0110.001

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 head0.016
GPT teacher head0.268
Teacher spread0.251 · 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; both teacher heads agree on what is shown here.

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

Citations43
Published2001
Admission routes1
Has abstractyes

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