{"@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/1360004229806348928.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2016jb013027"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2016JB013027"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2016JB013027"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Comparative study of tectonic tremor locations: Characterization of slow earthquakes in Guerrero, Mexico"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Deep tectonic tremor in Guerrero, Mexico, has been observed using dense temporal seismic networks (i.e., the Meso‐American Subduction Experiment and Guerrero Gap Experiment (G‐GAP) arrays) during two different time periods. We apply a set of seismic waveform analysis methods to these data sets to constrain the locations of tremors and determine the associated moment tensors. First we detect and locate the tremors. Next, very low frequency (VLF) signals are identified by stacking waveform data during tremor bursts, and their moment tensors are determined. Finally, to better investigate the link between tremors and VLF earthquakes, we detect VLF events using a matched filtering algorithm to search continuous seismic records. None of the 11 VLF events detected by this method occurred in the absence of tremor bursts suggesting they are indeed part of the same phenomena. Unlike previous investigations, our results for the G‐GAP period reveal that downdip tremor activity (i.e., in the so‐called “sweet spot”) is segmented into two patches separated by 40 km in the along‐trench direction, indicating possible variations in the geometry of the plate interface and/or slab effective pressure. Moment tensors of VLF signals are consistent with shear slip on the near‐horizontal plate interface, but source depths are about 5 km deeper than the established plate interface. The slip directions of the VLF events are slightly (~10°) counterclockwise of the plate convergence direction, indicating that strain energy promoting left‐lateral strike‐slip motion may accumulate in the continental crust during the interseismic period.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004229806348939","@type":"Researcher","foaf:name":[{"@value":"J. Maury"}],"jpcoar:affiliationName":[{"@value":"Earth and Planetary Science University of Tokyo Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229806349199","@type":"Researcher","foaf:name":[{"@value":"S. Ide"}],"jpcoar:affiliationName":[{"@value":"Earth and Planetary Science University of Tokyo Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380298336586497024","@type":"Researcher","foaf:name":[{"@value":"V. M. Cruz‐Atienza"}],"jpcoar:affiliationName":[{"@value":"Instituto de Geofísica Universidad Nacional Autónoma de México Mexico City Mexico"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229806349065","@type":"Researcher","foaf:name":[{"@value":"V. Kostoglodov"}],"jpcoar:affiliationName":[{"@value":"Instituto de Geofísica Universidad Nacional Autónoma de México Mexico City Mexico"}]},{"@id":"https://cir.nii.ac.jp/crid/1380298336586497025","@type":"Researcher","foaf:name":[{"@value":"G. González‐Molina"}],"jpcoar:affiliationName":[{"@value":"Instituto de Geofísica Universidad Nacional Autónoma de México Mexico City Mexico"}]},{"@id":"https://cir.nii.ac.jp/crid/1380298336586497153","@type":"Researcher","foaf:name":[{"@value":"X. Pérez‐Campos"}],"jpcoar:affiliationName":[{"@value":"Instituto de Geofísica Universidad Nacional Autónoma de México Mexico City Mexico"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"21699313"},{"@type":"EISSN","@value":"21699356"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2016-07","prism:volume":"121","prism:number":"7","prism:startingPage":"5136","prism:endingPage":"5151"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2016JB013027"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2016JB013027"}],"createdAt":"2016-07-09","modifiedAt":"2024-06-18","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781895907200","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"16H02219"},{"@type":"JGN","@value":"JP16H02219"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-16H02219/"}],"notation":[{"@language":"ja","@value":"世界の沈み込み帯における低速＆高速地震のダイナミクスの解明"},{"@language":"en","@value":"Dynamics of slow and fast earthqaukes in subduction zones worldwide"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000781902869376","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"16H06477"},{"@type":"JGN","@value":"JP16H06477"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PLANNED-16H06477/"}],"notation":[{"@language":"ja","@value":"低速変形から高速すべりまでの地球科学的モデル構築"},{"@language":"en","@value":"Study on Geoscientific Modeling of Earthquake Phenomena from Low-speed Deformation to High-speed Slip"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050564285755917184","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Nonvolcanic tremor observed in the Mexican subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002214348947712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Universality of slow earthquakes in the very low frequency 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