{"@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/1363670318526299520.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1038/sdata.2018.182"}},{"identifier":{"@type":"URI","@value":"https://www.nature.com/articles/sdata2018182.pdf"}},{"identifier":{"@type":"URI","@value":"https://www.nature.com/articles/sdata2018182"}},{"identifier":{"@type":"URI","@value":"http://www.nature.com/articles/sdata2018182"}}],"dc:title":[{"@value":"Seafloor crustal deformation data along the subduction zones around Japan obtained by GNSS-A observations"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Crustal deformation data obtained by geodetic observation networks are foundations in the fields of geodesy and seismology. These data are essential for understanding plate motion and earthquake sources and for simulating earthquake and tsunami scenarios. Although relatively scarce, seafloor geodetic data are particularly important for monitoring the behaviour of undersea interplate boundary regions. Since the mid-1990s, we have been developing the combined Global Navigation Satellite System-Acoustic ranging (GNSS-A) technique for realizing seafloor geodesy. This technique allows us to collect time series of seafloor crustal deformation. Our published data can be used to investigate several seismological phenomena along the subduction zones around Japan, namely the Nankai Trough, Sagami Trough and Japan Trench. These regions are globally important places in geodesy and seismology and are also suitable for comparison with other geophysical datasets. Our intention is for these data to promote further understanding of megathrust zones.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670318526299521","@type":"Researcher","foaf:name":[{"@value":"Yusuke Yokota"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318526299522","@type":"Researcher","foaf:name":[{"@value":"Tadashi Ishikawa"}]},{"@id":"https://cir.nii.ac.jp/crid/1410009221493277184","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000254627861"},{"@type":"NRID","@value":"9000254627694"},{"@type":"NRID","@value":"9000411809901"},{"@type":"NRID","@value":"9000403545230"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/Shun-ichi_WATANABE"}],"foaf:name":[{"@value":"Shun-ichi Watanabe"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"20524463"}],"prism:publicationName":[{"@value":"Scientific Data"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2018-09-11","prism:volume":"5","prism:number":"1","prism:startingPage":"180182"},"reviewed":"false","dc:rights":["https://creativecommons.org/licenses/by/4.0","https://creativecommons.org/licenses/by/4.0"],"url":[{"@id":"https://www.nature.com/articles/sdata2018182.pdf"},{"@id":"https://www.nature.com/articles/sdata2018182"},{"@id":"http://www.nature.com/articles/sdata2018182"}],"createdAt":"2018-09-11","modifiedAt":"2025-07-07","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050293710890939264","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Azimuthal differences and changes in strain rate and stress of the Japanese Islands deduced from geophysical data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360005518171998976","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Offshore Postseismic Deformation of the 2011 Tohoku Earthquake Revisited: Application of an Improved GPS‐Acoustic Positioning Method Considering Horizontal Gradient of Sound Speed Structure"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142423994240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A Decade of Lessons Learned from the 2011 Tohoku‐Oki Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142745248640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Development of a Trans‐Dimensional Fault Slip Inversion for Geodetic Data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021390741906432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatiotemporal distributions of afterslip and locking on the plate interface associated with the 2011 Tohoku-Oki earthquake using a 3-D temperature and strain rate-dependent heterogeneous viscosity model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360022304973152384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"On the use of tsunami-source data for high-resolution fault imaging of offshore earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360022306717165696","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Experimental verification of seafloor crustal deformation observations by UAV-based GNSS- A"}]},{"@id":"https://cir.nii.ac.jp/crid/1360022497406926848","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stress change in southwest Japan due to the 1944–1946 Nankai megathrust rupture sequence based on a 3-D heterogeneous rheological model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025431099443584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Numerical experiment toward simultaneous estimation of the spatiotemporal evolution of interseismic fault slips and block motions in southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643736032512","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Bayesian Inversion for a Stress‐Driven Model of Afterslip and Viscoelastic Relaxation: Method and Application to Postseismic Deformation Following the 2011 <i>M</i><sub><i>W</i></sub> 9.0 Tohoku‐Oki Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302865723788672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Representation and interpretation about underwater sound speed gradient field in the GNSS-A observation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306905612906752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Acoustic ambiguity reduction (AAR) method: an acoustic signal identification method for GNSS-A observation considering instrumental signal distortion"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092882858240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Kilometer-Scale Sound Speed Structure That Affects GNSS-A Observation: Case Study off the Kii Channel"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580230583896832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Temporal Change of km‐Scale Underwater Sound Speed Structure and GNSS‐A Positioning Accuracy"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580232173977472","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"An approximate travel time calculation and a robust GNSS-acoustic positioning method using an MCMC technique"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567859565440","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"History of On-Board Equipment Improvement for GNSS-A Observation With Focus on Observation Frequency"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567859575168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"GARPOS: Analysis Software for the GNSS‐A Seafloor Positioning With Simultaneous Estimation of Sound Speed Structure"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861707157648384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Along-arc heterogeneous rheology inferred from post-seismic deformation of the 2011 Tohoku-oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865815491929984","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mechanically Coupled Areas on the Plate Interface in the Kanto Region, Central Japan, Generating Great Earthquakes and Slow-Slip Events"}]},{"@id":"https://cir.nii.ac.jp/crid/1390298355913546496","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Steady Crustal Deformation Around Cape Omaezaki Revealed by InSAR Time Series Analysis Method"},{"@language":"ja","@value":"干渉SAR時系列解析手法を用いた御前崎周辺の定常的な地殻変動"}]},{"@id":"https://cir.nii.ac.jp/crid/1390305721537050496","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"日向灘南部における大地震の多様な発生様式"},{"@language":"en","@value":"Variation in Occurrence Patterns of Large Earthquakes in the Southern Part of Hyuga-nada"},{"@language":"ja-Kana","@value":"ヒュウガナダ ナンブ ニ オケル ダイジシン ノ タヨウ ナ ハッセイ ヨウシキ"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367083669504","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Crustal deformation detection capability of the GNSS-A seafloor geodetic observation array (SGO-A), provided by Japan Coast Guard"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842066368640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Heterogeneous rheology of Japan subduction zone revealed by postseismic deformation of the 2011 Tohoku-oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317026713344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Improvement on spatial resolution of a coseismic slip distribution using postseismic geodetic data through a viscoelastic inversion"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1038/sdata.2018.182"},{"@type":"CROSSREF","@value":"10.1029/2018jb017135_references_DOI_Q5lEWOQBDIrjK6hesQukPfZUpO6"},{"@type":"CROSSREF","@value":"10.1029/2020rg000713_references_DOI_Q5lEWOQBDIrjK6hesQukPfZUpO6"},{"@type":"CROSSREF","@value":"10.1029/2020jb020991_references_DOI_Q5lEWOQBDIrjK6hesQukPfZUpO6"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2022.106971_references_DOI_Q5lEWOQBDIrjK6hesQukPfZUpO6"},{"@type":"CROSSREF","@value":"10.21203/rs.3.rs-2919255/v1_references_DOI_Q5lEWOQBDIrjK6hesQukPfZUpO6"},{"@type":"CROSSREF","@value":"10.1186/s40623-024-02009-4_references_DOI_Q5lEWOQBDIrjK6hesQukPfZUpO6"},{"@type":"CROSSREF","@value":"10.1029/2020jb021620_references_DOI_Q5lEWOQBDIrjK6hesQukPfZUpO6"},{"@type":"CROSSREF","@value":"10.2467/mripapers.71.1_references_DOI_Q5lEWOQBDIrjK6hesQukPfZUpO6"},{"@type":"CROSSREF","@value":"10.1186/s40623-023-01878-5_references_DOI_Q5lEWOQBDIrjK6hesQukPfZUpO6"},{"@type":"CROSSREF","@value":"10.1093/gji/ggae083_references_DOI_Q5lEWOQBDIrjK6hesQukPfZUpO6"},{"@type":"CROSSREF","@value":"10.1186/s40623-024-02050-3_references_DOI_Q5lEWOQBDIrjK6hesQukPfZUpO6"},{"@type":"CROSSREF","@value":"10.1186/s40623-020-01207-0_references_DOI_Q5lEWOQBDIrjK6hesQukPfZUpO6"},{"@type":"CROSSREF","@value":"10.3389/feart.2020.00331_references_DOI_Q5lEWOQBDIrjK6hesQukPfZUpO6"},{"@type":"CROSSREF","@value":"10.1029/2022ea002224_references_DOI_Q5lEWOQBDIrjK6hesQukPfZUpO6"},{"@type":"CROSSREF","@value":"10.1186/s40623-022-01701-7_references_DOI_Q5lEWOQBDIrjK6hesQukPfZUpO6"},{"@type":"CROSSREF","@value":"10.1186/s40645-021-00453-4_references_DOI_Q5lEWOQBDIrjK6hesQukPfZUpO6"},{"@type":"CROSSREF","@value":"10.1186/s40623-022-01740-0_references_DOI_Q5lEWOQBDIrjK6hesQukPfZUpO6"},{"@type":"CROSSREF","@value":"10.1186/s40645-023-00539-1_references_DOI_Q5lEWOQBDIrjK6hesQukPfZUpO6"},{"@type":"CROSSREF","@value":"10.3389/feart.2020.00150_references_DOI_Q5lEWOQBDIrjK6hesQukPfZUpO6"},{"@type":"CROSSREF","@value":"10.3389/feart.2020.597532_references_DOI_Q5lEWOQBDIrjK6hesQukPfZUpO6"},{"@type":"CROSSREF","@value":"10.1093/gji/ggac063_references_DOI_Q5lEWOQBDIrjK6hesQukPfZUpO6"},{"@type":"CROSSREF","@value":"10.1038/s41598-023-31214-6_references_DOI_Q5lEWOQBDIrjK6hesQukPfZUpO6"},{"@type":"CROSSREF","@value":"10.1785/0120230073_references_DOI_Q5lEWOQBDIrjK6hesQukPfZUpO6"},{"@type":"CROSSREF","@value":"10.4294/zisin.2025-2s_references_DOI_Q5lEWOQBDIrjK6hesQukPfZUpO6"},{"@type":"CROSSREF","@value":"10.1186/s40623-023-01943-z_references_DOI_Q5lEWOQBDIrjK6hesQukPfZUpO6"}]}