MétaCan
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Slow slip near the trench at the Hikurangi subduction zone, New Zealand

2016· article· en· 332 citations· W2345518418 on OpenAlex· 10.1126/science.aaf2349

Why is this work in the frame?

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

Canadian funderA Canadian agency funded it. The work may carry no Canadian affiliation at all.

No Canadian affiliation. An affiliation-only frame, the usual design, would never have seen this work. It is one of the works that make the case for inverting the frame.

Classifier prediction

metacan-v1-d91a1de5be90

Predictions imitate two machine teachers. Scores are not calibrated prevalence probabilities.

Classifier candidate
ObservationalNot applicable
Classifier consensus
Observational
Teacher imitation scores

Codex

Other design0.812
Observational0.407
Not applicable0.005
Science and technology studies0.001
Theoretical or conceptual0.001
Bench or experimental0.001
Bibliometrics0.000
Research integrity0.000
Qualitative0.000
Open science0.000
Metaresearch0.000
Scholarly communication0.000
Simulation or modelling0.000
Randomized trial0.000
Case report0.000
Meta-epidemiology (narrow)0.000
Meta-epidemiology (broad)0.000
Non-randomized trial0.000
Meta-analysis0.000
Systematic review0.000

Gemma

Observational0.700
Not applicable0.442
Science and technology studies0.004
Theoretical or conceptual0.002
Bench or experimental0.001
Simulation or modelling0.001
Metaresearch0.001
Bibliometrics0.000
Open science0.000
Randomized trial0.000
Research integrity0.000
Case report0.000
Qualitative0.000
Meta-epidemiology (broad)0.000
Systematic review0.000
Meta-epidemiology (narrow)0.000
Scholarly communication0.000
Non-randomized trial0.000
Meta-analysis0.000

Machine scores (provisional)

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

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.

Opus teacher head0.015
GPT teacher head0.210
Teacher spread
0.195 how far apart the two teachers sit on this one work
Validation status
score_only:v0-immature-baseline verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Abstract

The range of fault slip behaviors near the trench at subduction plate boundaries is critical to know, as this is where the world's largest, most damaging tsunamis are generated. Our knowledge of these behaviors has remained largely incomplete, partially due to the challenging nature of crustal deformation measurements at offshore plate boundaries. Here we present detailed seafloor deformation observations made during an offshore slow-slip event (SSE) in September and October 2014, using a network of absolute pressure gauges deployed at the Hikurangi subduction margin offshore New Zealand. These data show the distribution of vertical seafloor deformation during the SSE and reveal direct evidence for SSEs occurring close to the trench (within 2 kilometers of the seafloor), where very low temperatures and pressures exist.

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