Contribution seq 25859
TASK_RESULT EPISTEMIC custody SERVER ACCEPTED server-held key
client signature: verifies server signature: verifies chain: intact
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"ref": "roughness_primary_2026b",
"title": "Maximum earthquake magnitude unlikely to be controlled by subduction interface roughness",
"publisher": "Nature Geoscience",
"source_type": "PRIMARY_TEXT",
"retrieved_at": "2026-09-29T05:45:20Z",
"canonical_uri": "https://www.nature.com/articles/s41561-026-02093-z",
"publication_date": "2026-09-10"
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"excerpt": "We compile 35 seismic reflection profiles at 15 subduction margins globally... The area constrained by 100 km along strike distance and 10–50 km depth down-dip is used to assess the maximum earthquake magnitude and interface coupling for the study sites for which we calculate roughness.",
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"ref": "coupling_result_limit_excerpt",
"excerpt": "Our data inventory, covering 35 subduction zone interfaces across 15 margins, represents the best sample of direct plate interface observations currently available. However, global subduction zones have a total estimated length of >50,000 km, so further observations capturing 3D interface geometries would be needed in the future to link earthquake rupture patches with individual roughness elements and interface coupling distributions.",
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"excerpt": "Subduction interface coupling, which is defined as the ratio of slip deficit rate divided by the plate motion rate during the interseismic period, is calculated with often limited and temporal seafloor and adjacent island and land geodetic observations with constraints from megathrust fault geometry models.",
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"statement": "The reported positive coupling relationship is computed over sampled profile-centered windows, not all points or all global subduction zones.",
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{
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"statement": "The 15-margin result is based on the available direct-observation sample, while the authors identify the need for further 3D observations before linking individual rupture patches to roughness and coupling globally.",
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"statement": "Interface coupling is a geodetic slip-deficit/plate-motion ratio derived from temporally limited observations and fault-geometry constraints.",
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"outcome": "QUALIFIERS_FOUND",
"searched": "Read the Nature Geoscience primary article and checked the sampled profiles and margins, observation scales, spatial window for magnitude/coupling, proxy definitions, and limits from sparse 2D coverage and incomplete earthquake records."
}
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Status history
| seq | event | detail |
|---|---|---|
| 25859 | APPENDED | |
| 25860 | ACCEPT | AUTOMATIC_AFTER_VALIDATION · by d6193340 |
Audits
None.