{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1361137045906040960.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2011gl048319"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2011GL048319"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2011GL048319"}}],"dc:title":[{"@value":"Deep tremor in New Zealand triggered by the 2010 Mw8.8 Chile earthquake"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Deep non‐volcanic tremor (NVT) is usually associated with episodic slow‐slip events. New Zealand is one notable exception where numerous slow slip events have been identified, yet NVT has remained undetected. Here we present the first known case of triggered NVT at New Zealand's Hikurangi subduction margin. Following the Mw8.8 Chilean earthquake of February 27, 2010, we identify coherent high‐frequency tremor signals that are in phase with, and modulated by, the passing Rayleigh waves. This is consistent with the surface wave triggering potential for strike‐normal incidence on a low‐angle thrust fault. After constraining the tremor depth on the plate interface, we locate the tremor source within 20 km of the source area of episodic slow slip. The tremor location is also near the edge of a region with high seismic attenuation that marks the boundary between dehydrated subducted slab and inferred hydrated, underplated sediment. We speculate that reduced interface friction and high fluid pressures provided by fluid‐rich underplated sediment facilitates the tremor generation.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380294643696248716","@type":"Researcher","foaf:name":[{"@value":"B. Fry"}],"jpcoar:affiliationName":[{"@value":"GNS Science  Lower Hutt New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137045906040964","@type":"Researcher","foaf:name":[{"@value":"K. Chao"}],"jpcoar:affiliationName":[{"@value":"School of Earth and Atmospheric Sciences Georgia Institute of Technology  Atlanta Georgia USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137045906040960","@type":"Researcher","foaf:name":[{"@value":"S. Bannister"}],"jpcoar:affiliationName":[{"@value":"GNS Science  Lower Hutt New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137045906040961","@type":"Researcher","foaf:name":[{"@value":"Z. Peng"}],"jpcoar:affiliationName":[{"@value":"School of Earth and Atmospheric Sciences Georgia Institute of Technology  Atlanta Georgia USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137045906040963","@type":"Researcher","foaf:name":[{"@value":"L. Wallace"}],"jpcoar:affiliationName":[{"@value":"GNS Science  Lower Hutt New Zealand"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"EISSN","@value":"19448007"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2011-08","prism:volume":"38","prism:number":"15","prism:startingPage":"L15306"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2011GL048319"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2011GL048319"}],"createdAt":"2011-08-05","modifiedAt":"2023-09-14","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050282677821468672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Bayesian approach for detecting dynamically triggered very low-frequency earthquakes in the Nankai subduction zone and application to the 2016 Mw5.9 off-Kii Peninsula earthquake, Japan"},{"@value":"Erratum: Bayesian approach for detecting dynamically triggered very low-frequency earthquakes in the Nankai subduction zone and application to the 2016 Mw 5.9 off-Kii Peninsula earthquake, Japan"},{"@value":"Bayesian approach for detecting dynamically triggered very low-frequency earthquakes in the Nankai subduction zone and application to the 2016<i>M</i>w 5.9 off-Kii Peninsula earthquake, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1050852327888050304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tectonic tremors in the Northern Mexican subduction zone remotely triggered by the 2017 Mw8.2 Tehuantepec earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233292223744","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Earthquakes and Tremor Linked to Seamount Subduction During Shallow Slow Slip at the Hikurangi Margin, New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142902736512","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Isolated Triggered Tremor Spots in South America and Implications for Global Tremor Activity"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285708266738944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"New detection of tremor triggered in Hokkaido, northern Japan by the 2004 Sumatra–Andaman earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285708269022720","@type":"Article","resourceType":"学術雑誌論文(journal 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