{"@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/1363670321132848512.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2019gl085303"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2019GL085303"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GL085303"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2019GL085303"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2019GL085303"}}],"dc:title":[{"@value":"A Long‐Term View of Episodic Tremor and Slip in Cascadia"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Episodic Tremor and Slip, or ETS, is a well‐recognized phenomenon in the Cascadia subduction zone. Constraining the precise location of geodetically measured slip during ETS is important for clarifying the relationship between slip and tremor during ETS, the location of ETS slip relative to the strongly locked zone, and the role of ETS in the overall slip budget. Here I present a new method for separating Global Navigation Satellite System time series in Cascadia into ETS and inter‐ETS components, deriving long‐term average ETS velocities for each site. These velocities are then inverted for a time‐averaged ETS slip rate on the plate interface. I find that ETS and its role in the slip budget are highly variable and segmented along strike. This inversion represents the highest‐resolution image of the ETS zone derived from geodetic data to date. Slip correlates well with tremor locations, and a possible second updip ETS zone is detected.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670321132848384","@type":"Researcher","foaf:name":[{"@value":"Noel M. Bartlow"}],"jpcoar:affiliationName":[{"@value":"Berkeley Seismological Laboratory University of California  Berkeley CA USA"}]}],"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":"2020-02-05","prism:volume":"47","prism:number":"3","prism:startingPage":"e2019GL085303"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2019GL085303"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GL085303"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2019GL085303"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2019GL085303"}],"createdAt":"2020-01-24","modifiedAt":"2025-06-02","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050287606237344896","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Detailed Spatial Slip Distribution for Short‐Term Slow Slip Events Along the Nankai Subduction Zone, Southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1050572244954692224","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Slow Slip Events in the Kanto and Tokai Regions of Central Japan Detected Using Global Navigation Satellite System Data During 1994–2020"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168721882240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effects of episodic slow slip on seismicity and stress near a subduction-zone megathrust"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017282189457792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Segmentation of Shallow Slow Slip Events at the Hikurangi Subduction Zone Explained by Along‐Strike Changes in Fault Geometry and Plate Convergence Rates"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017282190564608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Imaging evolution of Cascadia slow-slip event using high-rate GPS"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025430178098816","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Slip‐Tremor Interaction at the Very Beginning of Episodic Tremor and Slip in Cascadia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292618543890432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The generation of large earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580230583868544","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"<i>l</i>\n                    <sub>1</sub>\n                    Trend Filtering‐Based Detection of Short‐Term Slow Slip Events: Application to a GNSS Array in Southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865815689043456","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Recent advances in earthquake seismology using machine learning"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842051749120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Detection of deep low-frequency earthquakes in the Nankai subduction zone over 11 years using a matched filter technique"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2019gl085303"},{"@type":"CROSSREF","@value":"10.1038/s43017-020-00108-w_references_DOI_NCHYv6t2urYXkwQxw7GsQM57OiE"},{"@type":"CROSSREF","@value":"10.1038/s41467-021-27453-8_references_DOI_NCHYv6t2urYXkwQxw7GsQM57OiE"},{"@type":"CROSSREF","@value":"10.1029/2021jb022913_references_DOI_NCHYv6t2urYXkwQxw7GsQM57OiE"},{"@type":"CROSSREF","@value":"10.1038/s41598-022-10957-8_references_DOI_NCHYv6t2urYXkwQxw7GsQM57OiE"},{"@type":"CROSSREF","@value":"10.1029/2024av001425_references_DOI_NCHYv6t2urYXkwQxw7GsQM57OiE"},{"@type":"CROSSREF","@value":"10.1029/2020jb019613_references_DOI_NCHYv6t2urYXkwQxw7GsQM57OiE"},{"@type":"CROSSREF","@value":"10.1029/2021jb023258_references_DOI_NCHYv6t2urYXkwQxw7GsQM57OiE"},{"@type":"CROSSREF","@value":"10.1029/2020gc009329_references_DOI_NCHYv6t2urYXkwQxw7GsQM57OiE"},{"@type":"CROSSREF","@value":"10.1186/s40623-020-01257-4_references_DOI_EHQuVdQ83MWRHpaQqgRcEGzQja6"},{"@type":"CROSSREF","@value":"10.1186/s40623-024-01982-0_references_DOI_EHQuVdQ83MWRHpaQqgRcEGzQja6"}]}