{"@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/1360002216175330176.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.tecto.2012.08.022"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0040195112004994?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0040195112004994?httpAccept=text/plain"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Episodic slow slip events in the Japan subduction zone before the 2011 Tohoku-Oki earthquake"}],"description":[{"notation":[{"@value":"Abstract   We describe two transient slow slip events that occurred before the 2011 Tohoku-Oki earthquake. The first transient crustal deformation, which occurred over a period of a week in November 2008, was recorded simultaneously using ocean-bottom pressure gauges and an on-shore volumetric strainmeter; this deformation has been interpreted as being an M6.8 episodic slow slip event. The second had a duration exceeding 1 month and was observed in February 2011, just before the 2011 Tohoku-Oki earthquake; the moment magnitude of this event reached 7.0. The two events preceded interplate earthquakes of magnitudes M6.1 (December 2008) and M7.3 (March 9, 2011), respectively; the latter is the largest foreshock of the 2011 Tohoku-Oki earthquake. Our findings indicate that these slow slip events induced increases in shear stress, which in turn triggered the interplate earthquakes. The slow slip event source area on the fault is also located within the downdip portion of the huge-coseismic-slip area of the 2011 earthquake. This demonstrates episodic slow slip and seismic behavior occurring on the same portions of the megathrust fault, suggesting that the faults undergo slip in slow slip events can also rupture seismically."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380847869285078925","@type":"Researcher","foaf:name":[{"@value":"Yoshihiro Ito"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869285078922","@type":"Researcher","foaf:name":[{"@value":"Ryota Hino"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869285078915","@type":"Researcher","foaf:name":[{"@value":"Motoyuki Kido"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869285078919","@type":"Researcher","foaf:name":[{"@value":"Hiromi Fujimoto"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869285078923","@type":"Researcher","foaf:name":[{"@value":"Yukihito Osada"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869285078913","@type":"Researcher","foaf:name":[{"@value":"Daisuke Inazu"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869285078920","@type":"Researcher","foaf:name":[{"@value":"Yusaku Ohta"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869285078924","@type":"Researcher","foaf:name":[{"@value":"Takeshi Iinuma"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869285078916","@type":"Researcher","foaf:name":[{"@value":"Mako Ohzono"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869285078917","@type":"Researcher","foaf:name":[{"@value":"Satoshi Miura"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869285078921","@type":"Researcher","foaf:name":[{"@value":"Masaaki Mishina"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869285078918","@type":"Researcher","foaf:name":[{"@value":"Kensuke Suzuki"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869285078914","@type":"Researcher","foaf:name":[{"@value":"Takeshi Tsuji"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869285078912","@type":"Researcher","foaf:name":[{"@value":"Juichiro Ashi"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00401951"},{"@type":"PISSN","@value":"https://id.crossref.org/issn/00401951"}],"prism:publicationName":[{"@value":"Tectonophysics"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2013-07","prism:volume":"600","prism:startingPage":"14","prism:endingPage":"26"},"reviewed":"false","url":[{"@id":"https://api.elsevier.com/content/article/PII:S0040195112004994?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0040195112004994?httpAccept=text/plain"}],"createdAt":"2012-08-24","modifiedAt":"2023-06-25","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000782062678912","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"21107007"},{"@type":"JGN","@value":"JP21107007"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PLANNED-21107007/"}],"notation":[{"@language":"ja","@value":"海溝型巨大地震の準備・発生過程のモデル構築"},{"@language":"en","@value":"Comprehensive modeling of pre- and co-seismic processes"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257006915328","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"20244070"},{"@type":"JGN","@value":"JP20244070"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-20244070/"}],"notation":[{"@language":"ja","@value":"海底測地・地震観測に基づくマルチスケールゆっくり地震の検出"},{"@language":"en","@value":"Multi-scale types of slow earthquakes based on ocean-bottom geodetic and seismological observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257039322624","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"21107003"},{"@type":"JGN","@value":"JP21107003"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PLANNED-21107003/"}],"notation":[{"@language":"ja","@value":"高精度変動地形・地質調査による巨大地震断層の活動履歴の解明"},{"@language":"en","@value":"High precision topographical/geological surveys for elucidating the activity history of seismogenic faults"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257110790656","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"22740287"},{"@type":"JGN","@value":"JP22740287"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-22740287/"}],"notation":[{"@language":"ja","@value":"複合測地学データに基づく奥羽脊梁山脈直下のレオロジー構造に関する研究"},{"@language":"en","@value":"Research of rheological structure beneath the Ou-backbone Range based on the multiple geodetic data"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001202560213760","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Spectrum of slip behaviour in Tohoku fault zone samples at plate tectonic slip rates"}]},{"@id":"https://cir.nii.ac.jp/crid/1050001338452605568","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Development of a Slow Earthquake Database"}]},{"@id":"https://cir.nii.ac.jp/crid/1050001339107234432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Connecting slow earthquakes to huge earthquakes"},{"@value":"Connecting slow earthquakes to large earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1050006065615081472","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stress release process along an intraplate fault analogous to the plate boundary: a case study of the 2017 M5.2 Akita-Daisen earthquake, NE Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1050009295028707584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Earthquake Swarm Detection Along the Hikurangi Trench, New Zealand: Insights Into the Relationship Between Seismicity and Slow Slip Events"}]},{"@id":"https://cir.nii.ac.jp/crid/1050013474495795840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A review on slow earthquakes in the Japan Trench"}]},{"@id":"https://cir.nii.ac.jp/crid/1050015333084080512","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Effects of the Tsunami Generated by the 1662 Hyuga-Nada Earthquake off Miyazaki Prefecture, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1050017832012437632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Physical Mechanism for a Temporal Decrease of the Gutenberg-Richter b-Value Prior to a Large Earthquake"},{"@value":"Physical Mechanism for a Temporal Decrease of the Gutenberg‐Richter <i>b</i>‐Value Prior to a Large Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1050282677887377024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatiotemporal Evolution of Recurrent Slow Slip Events Along the Southern Ryukyu Subduction Zone, Japan, From 2010 to 2013"}]},{"@id":"https://cir.nii.ac.jp/crid/1050282810792973312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Episodic tremor and slip near the Japan Trench prior to the 2011 Tohoku-Oki earthquake"},{"@value":"Episodic tremor and slip near the Japan Trench prior to the 2011 Tohoku‐Oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1050285299888364800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Episodic tremor and slip silently invades strongly locked megathrust in the Nankai Trough"}]},{"@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/1050292561229551360","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Water Depth Dependence of Long‐Range Correlation in Nontidal Variations in Seafloor Pressure"},{"@value":"Water depth dependence of long-range correlation in nontidal variations in seafloor pressure"}]},{"@id":"https://cir.nii.ac.jp/crid/1050566774865074816","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Possible slow slip event beneath the Kii Peninsula, southwest Japan, inferred from historical tilt records in 1973"}]},{"@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/1050577972975048832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Development of an Epidemic‐type Aftershock‐sequence Model Explicitly Incorporating the Seismicity‐triggering Effects of Slow Slip Events"},{"@value":"Development of an epidemic-type aftershock-sequence model explicitly incorporating the seismicity-triggering effects of slow slip events"}]},{"@id":"https://cir.nii.ac.jp/crid/1050845760675301632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Frontal wedge deformation near the source region of the 2011 Tohoku-Oki earthquake"},{"@value":"Frontal wedge deformation near the source region of the 2011 Tohoku‐Oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1050845760694761856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Potential tsunamigenic faults of the 2011 off the Pacific coast of Tohoku Earthquake"},{"@value":"Potential tsunamigenic faults of the 2011 Tohoku earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1050863550659700608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Did Short-Term Preseismic Crustal Deformation Precede the 2011 Great Tohoku-Oki Earthquake? An Examination of Stacked Tilt Records"},{"@value":"Did Short‐Term Preseismic Crustal Deformation Precede the 2011 Great Tohoku‐Oki Earthquake? An Examination of Stacked Tilt Records"}]},{"@id":"https://cir.nii.ac.jp/crid/1050866117150510336","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Deep plutonic bodies over low-frequency earthquakes revealed from receiver-side Green's functions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360001113984120704","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Shallow Low‐Frequency Tremor in the Northern Japan Trench Subduction Zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002214349012992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Under what circumstances does a seismogenic patch produce aseismic transients in the later interseismic period?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002214351275136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Frictional properties of JFAST core samples and implications for slow earthquakes at the Tohoku subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229801884928","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Boso slow slip events in 2007 and 2011 as a driving process for the accompanying earthquake swarm"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229806477824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Near‐field observations of an offshore <i>M<sub>w</sub></i> 6.0 earthquake from an integrated seafloor and subseafloor monitoring network at the Nankai Trough, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229807698176","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Detection of vertical motion during a slow‐slip event off the Boso Peninsula, Japan, by ocean bottom pressure gauges"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229807707136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Temporal variation of intermediate‐depth earthquakes around the time of the <i>M</i>9.0 Tohoku‐oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232135292416","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Extension of continental crust by anelastic deformation during the 2011 Tohoku-oki earthquake: The role of extensional faulting in the generation of a great tsunami"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232135547264","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"3D geometry of a plate boundary fault related to the 2016 Off-Mie earthquake in the Nankai subduction zone, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232523514496","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Strain rate effect on fault slip and rupture evolution: Insight from meter-scale rock friction experiments"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233291826432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seafloor Crustal Deformation on Ocean Bottom Pressure Records With Nontidal Variability Corrections: Application to Hikurangi Margin, New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004235955794048","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Slow slip near the trench at the Hikurangi subduction zone, New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004236002955136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Learning from crustal deformation associated with the M9 2011 Tohoku-oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004236864452736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Ocean bottom pressure records of the 2011 Tohoku-Oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004238190841984","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A Seismogeodetic Amphibious Network in the Guerrero Seismic Gap, Mexico"}]},{"@id":"https://cir.nii.ac.jp/crid/1360005518173396992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Comprehensive Detection of Very Low Frequency Earthquakes Off the Hokkaido and Tohoku Pacific Coasts, Northeastern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360005520966852736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The slow earthquake spectrum in the Japan Trench illuminated by the S-net seafloor observatories"}]},{"@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/1360011142931996288","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Effective resolution and drift of Paroscientific pressure sensors derived from long‐term seafloor measurements"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142940259072","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Free software helps map and display data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144195146752","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A procedure for tidal analysis with a Bayesian information criterion"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168737955200","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Foreshock Activity Promoted by Locally Elevated Loading Rate on a 4‐m‐Long Laboratory Fault"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013170949096064","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Continuous GPS Array and Present-day Crustal Deformation of Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360016870443278592","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Abrupt water temperature increases near seafloor during the 2011 Tohoku earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017282206787968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Influence of shear zone thickness and strike-slip faulting on tectonic tremor in the Nankai Trough, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021395469197056","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Progress in modeling the Tohoku-oki megathrust earthquake cycle and associated crustal deformation processes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025033655478272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Revisiting Slip Deficit Rates and Its Insights Into Large and Slow Earthquakes at the Nankai Subduction Zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025430208867072","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Investigation on short-term slow slip events in the northeast Japan subduction zones using decadal GNSS data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025431094351872","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatiotemporal evolution of a deep short-term slow slip event in the Nankai subduction zone in November 2022 derived from strain, tilt, and GNSS records"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283689326464256","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Nucleation of frictional instability caused by fluid pressurization in subducted blueschist"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283690387835648","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The detectability of shallow slow earthquakes by the Dense Oceanfloor Network system for Earthquakes and Tsunamis (DONET) in Tonankai district, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283691685598592","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Trench-normal variation in observed seafloor displacements associated with the 2011 Tohoku-Oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283691686407040","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Coseismic slip distribution of the 2011 off the Pacific Coast of Tohoku Earthquake (M9.0) refined by means of seafloor geodetic data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283693415157376","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The 2011 Tohoku-Oki Earthquake: Displacement Reaching the Trench Axis"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283693426062080","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Periodic slow slip triggers megathrust zone earthquakes in northeastern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704784584448","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Coseismic slip propagation on the Tohoku plate boundary fault facilitated by slip‐dependent weakening during slow fault slip"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704785143680","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Detection of earthquake swarms at subduction zones globally: Insights into tectonic controls on swarm activity"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285705099046400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Changes in electrical resistivity track changes in tectonic plate coupling"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285708269006208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatiotemporal Variation of Tectonic Tremor Activity Before the Tohoku‐Oki Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285715178541696","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"IODP workshop: Core-Log Seismic Investigation at Sea – Integrating legacy data to address outstanding research questions in the Nankai Trough Seismogenic  Zone Experiment"}]},{"@id":"https://cir.nii.ac.jp/crid/1360286993149768192","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Migrations and Clusters of Shallow Very Low Frequency Earthquakes in the Regions Surrounding Shear Stress Accumulation Peaks Along the Nankai Trough"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617400394880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Deep slow-slip events promote seismicity in northeastern Japan megathrust"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617861149056","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismic energy radiation and along-strike heterogeneities of shallow tectonic tremors at the Nankai Trough and Japan Trench"}]},{"@id":"https://cir.nii.ac.jp/crid/1360291932833460480","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mobile Pressure Calibrator for the Development of Submarine Geodetic Monitoring Systems"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617909770624","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Nonvolcanic Deep Tremor Associated with Subduction in Southwest Japan"}]},{"@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/1360292619426814208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Repeating earthquakes and interplate aseismic slip in the northeastern Japan subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619929471744","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Effect of recent revisions to the geomagnetic reversal time scale on estimates of current plate motions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292621074223104","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"EVIDENCE FOR ASEISMIC DEFORMATION RATE CHANGES PRIOR TO EARTHQUAKES"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292621180573568","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mechanism of tsunami earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292621388170624","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Surface deformation due to shear and tensile faults in a half-space"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643770209920","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Editorial: Frontiers in Seafloor Geodesy"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643805703424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Influence of structure and pore pressure of plate interface on tectonic tremor in the Nankai subduction zone, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298337112216320","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stick-slip behavior of a clayey crustal fault"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298754805115008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Modeling of earthquake-induced landslide distributions based on the active fault parameters"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302865743074304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effects of phyllosilicate content on the slip behavior of fault gouge: Insights from room-temperature friction experiments on quartz–talc mixtures"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306904387869184","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatiotemporal Evolution of Slow Slip Events at the Offshore Hikurangi Subduction Zone in 2019 Using GNSS, InSAR, and Seafloor Geodetic Data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165364548608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Was the 2011 Tohoku-Oki earthquake preceded by aseismic preslip? Examination of seafloor vertical deformation data near the epicenter"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165997922688","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatiotemporal characteristics of the geomagnetic diurnal variation anomalies prior to the 2011 Tohoku earthquake (Mw 9.0) and the possible coupling of multiple pre-earthquake phenomena"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166662283776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Friction velocity dependence of clay-rich fault material along a megasplay fault in the Nankai subduction zone at intermediate to high velocities"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179757322752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Velocity‐ and slip‐dependent weakening in simulated fault gouge: Implications for multimode fault slip"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182088656640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Silica diagenesis and its effect on interplate seismicity in cold subduction zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567183240083328","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A slip pulse model with fault heterogeneity for low‐frequency earthquakes and tremor along plate interfaces"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567183243391488","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geodetic constraints on afterslip characteristics following the March 9, 2011, Sanriku‐oki earthquake, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567183246660992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tremor and Inferred Slow Slip Associated With Afterslip of the 2011 Tohoku Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567186250363776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Global Positioning System (GPS) and GPS-Acoustic Observations: Insight into Slip Along the Subduction Zones Around Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360568468306041984","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tomography of the source zone of the great 2011 Tohoku earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360568693011161216","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Shallow Nonvolcanic Tremor Activity and Potential Repeating Earthquakes in the Chile Triple Junction: Seismic Evidence of the Subduction of the Active Nazca–Antarctic Spreading Center"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092737492864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Improving Detectability of Seafloor Deformation From Bottom Pressure Observations Using Numerical Ocean Models"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092884419328","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Episodic slow slip events accompanied by non‐volcanic tremors in southwest Japan subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092886258944","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Low-frequency earthquakes in Shikoku, Japan, and their relationship to episodic tremor and slip"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092891528064","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Displacement Above the Hypocenter of the 2011 Tohoku-Oki Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095880367488","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Continuous Long-Term Seafloor Pressure Observation for Detecting Slow-Slip Interplate Events in Miyagi-Oki on the Landward Japan Trench Slope"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118672522880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatial relationship between shallow very low frequency earthquakes and the subducted Kyushu-Palau Ridge in the Hyuga-nada region of the Nankai subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118747835648","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Shallow Slow Earthquake Episodes Near the Trench Axis off Costa Rica"}]},{"@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/1360584339757736448","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Reduction of non-tidal oceanographic fluctuations in ocean-bottom pressure records of DONET using principal component analysis to enhance transient tectonic detectability"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584339757796352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Incoming plate structure at the Japan Trench subduction zone revealed in densely spaced reflection seismic profiles"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584340508721536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatiotemporal Distribution of Shallow Tremors Along the Nankai Trough, Southwest Japan, as Determined From Waveform Amplitudes and Cross‐Correlations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360585254927006848","@type":"Article","resourceType":"preprint","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Reduction of non-tidal oceanographic fluctuations in ocean bottom pressure records of DONET using principal component analysis to enhance tectonic transient detectability"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588381062523520","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Estimating Vertical Movement and Slip Distribution During the 2018 Boso, Japan, Slow Slip Event From Ocean Bottom Pressure Gauge Data and an Oceanic Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846639280836480","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Active thrusting of the Longquan Fault in the central Sichuan basin, China, and the seismotectonic behavior in the Longmen Shan fold‐and‐thrust belt"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846643368612224","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Propagation of Slow Slip Leading Up to the 2011\n            <i>M</i>\n            <sub>w</sub>\n            9.0 Tohoku-Oki Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848654736707840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Temporal variation of tectonic tremor activity in southern Taiwan around the 2010 <i>M</i><sub><i>L</i></sub>6.4 Jiashian earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848655105468416","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Slow slip and aseismic deformation episodes associated with the subducting Pacific plate offshore Japan, revealed by changes in seismicity"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848656073912832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Quasi-Dynamic 3D Modeling of the Generation and Afterslip of a Tohoku-oki Earthquake Considering Thermal Pressurization and Frictional Properties of the Shallow Plate Boundary"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848658222216064","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Recurring Slow Slip Events and Earthquake Nucleation in the Source Region of the <i>M</i> 7 Ibaraki‐Oki Earthquakes Revealed by Earthquake Swarm and Foreshock Activity"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848659519867904","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"An approximately 9-yr-period variation in seismicity and crustal deformation near the Japan Trench and a consideration of its origin"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855568640541440","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Precise point positioning for the efficient and robust analysis of GPS data from large networks"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855571281879168","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Variability of Near-Term Probability for the Next Great Earthquake on the Cascadia Subduction Zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857593727558272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Propagation of a precursory detachment front along a seismogenic plate interface in a rate–state friction model of earthquake cycles"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861287035222144","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geodetic and Geological Deformation of the Island Arc in Northeast Japan Revealed by the 2011 Tohoku Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861704795763840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Connection between high pore-fluid pressure and frictional instability at tsunamigenic plate boundary fault of 2011 Tohoku-Oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861705590716416","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Temporal velocity variations in the northern Hikurangi margin and the relation to slow slip"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861707144100480","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tilt Observations at the Seafloor by Mobile Ocean Bottom Seismometers"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865815498582912","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Largest Aftershock Nucleation Driven by Afterslip During the 2014 Iquique Sequence"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869854370617472","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Community‐Driven Code Comparisons for Simulations of Fluid‐Induced Aseismic Slip"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869855567008768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Data assimilation for fault slip monitoring and short-term prediction of spatio-temporal evolution of slow slip events: application to the 2010 long-term slow slip event in the Bungo Channel, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869856028074496","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"New insight into slow earthquake activities from continuous ocean bottom seismometers at the Guerrero seismic gap, Mexico"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045060447616","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Diverse slow slip behavior at the Hikurangi subduction margin, New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045249909248","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Non-volcanic tremor associated with the March 2010 Gisborne slow slip event at the Hikurangi subduction margin, New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137046449020032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Slow earthquakes and great earthquakes along the Nankai trough"}]},{"@id":"https://cir.nii.ac.jp/crid/1361412896196728192","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The State of Stress on the Fault Before, During, and After a Major Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520750308480","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Coseismic and postseismic slip of the 2011 magnitude-9 Tohoku-Oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520977172352","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Deep-Ocean Bottom Pressure Measurement: Drift Removal and Performance"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699993624580864","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A comparison of in situ bottom pressure array measurements with GRACE estimates in the Kuroshio Extension"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699993742595584","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rupture process of the 9 March, 2011 Mw 7.4 Sanriku-Oki, Japan earthquake constrained by jointly inverting teleseismic waveforms, strong motion data and GPS observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995574436608","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"ITRF2008: an improved solution of the international terrestrial reference frame"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981469343259520","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The 2011 Magnitude 9.0 Tohoku-Oki Earthquake: Mosaicking the Megathrust from Seconds to Centuries"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981469536823040","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mapping Circulation in the Kuroshio Extension with an Array of Current and Pressure Recording Inverted Echo Sounders"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945481196288","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Possible deep fault slip preceding the 2004 Parkfield earthquake, inferred from detailed observations of tectonic tremor"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262946154287360","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A global barotropic ocean model driven by synoptic atmospheric disturbances for detecting seafloor vertical displacements from in situ ocean bottom pressure measurements"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544418722734080","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Spatiotemporal distribution of very-low frequency earthquakes in Tokachi-oki near the junction of the Kuril and Japan trenches revealed by using array signal processing"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420150290048","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Correlated transient fluid pulsing and seismic tremor in the Costa Rica subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420347007232","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Hydrologic detection and finite element modeling of a slow slip event in the Costa Rica prism toe"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420986062464","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Interplate Coupling in the Kanto District, Central Japan, and the Boso Peninsula Silent Earthquake in May 1996"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388843686032512","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A large slow slip event on the central Hikurangi subduction interface beneath the Manawatu region, North Island, New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844242379392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Episodic Tremor and Slip on the Cascadia Subduction Zone: The Chatter of Silent Slip"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845868670208","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Strategies for high‐precision Global Positioning System orbit determination"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670319089972224","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Silent fault slip following an interplate thrust earthquake at the Japan Trench"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320329608704","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Single receiver phase ambiguity resolution with GPS data"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951793447762816","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Earthquakes and friction laws"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951793876146816","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Slow slip events and seismic tremor at circum‐Pacific subduction zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233269991901952","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Slow Earthquakes Coincident with Episodic Tremors and Slow Slip Events"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233270426238080","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Silent Slip Event on the Deeper Cascadia Subduction Interface"}]},{"@id":"https://cir.nii.ac.jp/crid/1370849942246020742","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On the changes in the sea level at Tosashimizu before the Nankaido earthquake of 1946"}]},{"@id":"https://cir.nii.ac.jp/crid/1370849942246020868","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Crustal movements as earthquake precursors — leveling anomaly before the 1944 Tonankai earthquake revisited"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204146186880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"On Earthquake Prediction in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204147093760","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Modeling fast and slow earthquakes at various scales"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204306119040","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"断層力学·モデリングに基づく震源過程の多面的研究"},{"@language":"en","@value":"Source Processes Based on Fault Mechanics and Modeling"},{"@value":"断層力学・モデリングに基づく震源過程の多面的研究"},{"@language":"ja-Kana","@value":"ダンソウ リキガク ・ モデリング ニ モトズク シンゲン カテイ ノ タメンテキ ケンキュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206512583680","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Very low frequency earthquakes excited by the 2004 off the Kii peninsula earthquakes: A dynamic deformation process in the large accretionary prism"},{"@value":"Very low frequency earthquake excited by the 2004 off the Kii peninsula earthquake: a dynamic deformation process in the large accretionary prism"},{"@value":"Very low frequency earthquakes excited by the 2004 off Kii peninsula earthquakes: a dynamic deformation process in the large accretionary prism"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206513470848","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Silent earthquakes occurring in a stable-unstable transition zone and implications for earthquake prediction"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001288035936640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Achievements of the rapid response drilling (IODP Expedition 343: J-FAST) after the 2011 off the Pacific coast of Tohoku Earthquake"},{"@language":"ja","@value":"東北地方太平洋沖地震後の緊急調査掘削（IODP第343次航海：J-FAST）の成果"},{"@language":"ja-Kana","@value":"トウホク チホウ タイヘイヨウオキ ジシン ゴ ノ キンキュウ チョウサ クッサク(IODP ダイ343ジ コウカイ:J-FAST)ノ セイカ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001288150325376","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Contribution of Slow Earthquake Study for Assessing the Occurrence Potential of Megathrust Earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001288151363712","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Precursory Phenomena Possibly Related to the 2011 M9.0 Off the Pacific Coast of Tohoku Earthquake"},{"@value":"Precursory Phenomena Possibly Related to the 2011<i>M</i>9.0 Off the Pacific Coast of Tohoku Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679214265728","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"沈み込み帯におけるプレート境界面の不均質と地震活動"},{"@language":"en","@value":"Relationship between Heterogeneity of Plate Interface and Seismicity at Subduction Zones: The Japan Trench and Hikurangi Subduction Zones as Examples"},{"@value":"沈み込み帯におけるプレート境界面の不均質と地震活動 : 日本海溝およびヒクランギ沈み込み帯を例として"},{"@language":"ja-Kana","@value":"シズミ コミ タイ ニ オケル プレート キョウカイメン ノ フキンシツ ト ジシン カツドウ : ニホン カイコウ オヨビ ヒクランギ シズミ コミ タイ オ レイ ト シテ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679280917248","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"千葉県北部の地震活動と同期した非地震性すべり"},{"@language":"en","@value":"Aseismic Slips Synchronized with Earthquakes in Northern Chiba Prefecture, Central Japan"},{"@language":"ja-Kana","@value":"チバケン ホクブ ノ ジシン カツドウ ト ドウキ シタ ヒジシンセイスベリ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680087083648","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Sacks-Evertson Strainmeter, its installation in Japan and Some Preliminary Results Concerning Strain Steps"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489922688","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Low frequency events occurred during the sequence of aftershock activity of the 2003 Tokachi-Oki earthquake; a dynamic process of the tectonic erosion by subducted seamount"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681522422528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The influence of organic–rich shear zones on pelagic sediment deformation and seismogenesis in a subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1390283659860775680","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Main Results from the Program Promotion Panel for Subduction-Zone Earthquakes"}]},{"@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/1390567172587194752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Errata to “Characteristic activities of slow earthquakes in Japan”"},{"@value":"Characteristic activities of slow earthquakes in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390845713080982400","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Slow Slip Transients Before the 2011 Tohoku-Oki Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1390846609818226944","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Seafloor Geodetic Observations Decipher the 2011 Tohoku-Oki Earthquake"},{"@language":"ja","@value":"海底地殻変動観測で捉えた2011年東北地方太平洋沖地震"},{"@language":"ja-Kana","@value":"カイテイ チカク ヘンドウ カンソク デ トラエタ 2011ネン トウホク チホウ タイヘイヨウオキ ジシン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390870064891142656","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"東北地方太平洋岸において地形・地質学的に推定される地殻変動分布とその要因"},{"@language":"en","@value":"Distribution and causes of crustal deformation estimated from coastal geology along the Pacific coast, northeastern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1570009750829304960","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Low-frequency tremors associated with reverse faults in a shallow accretionary prism"},{"@value":"Low‐frequency tremors associated with reverse faults in a shallow accretionary prism"}]},{"@id":"https://cir.nii.ac.jp/crid/1572824501329363968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A scaling law for slow earthquakes"},{"@value":"A scaling law for slow earthqates"},{"@value":"A scaling law for slow earthquake"},{"@value":"A scaling low for slow earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417119872384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geological structures controlled the rupture process of the 2011 M9.0 Tohoku-Oki earthquake in the Northeast Japan Arc"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417136234368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Assessment of S-net seafoor pressure data quality in view of seafoor geodesy"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892090765696","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Ambient tectonic tremors in Manawatu, Cape Turnagain, Marlborough, and Puysegur, New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892138323712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Significant tsunami observed at ocean-bottom pressure gauges during the 2011 off the Pacific coast of Tohoku Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842042471296","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Variations in precursory slip behavior resulting from frictional heterogeneity"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842060077440","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A convolutional neural network-based classification of local earthquakes and tectonic tremors in Sanriku-oki, Japan, using S-net data"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842066365056","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Forecasting tectonic tremor activity using a renewal process model"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433316893073024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Distribution of low-frequency earthquakes accompanying the very low frequency earthquakes along the Ryukyu Trench"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317020017024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatio-temporal changes in the seismic velocity induced by the 2011 Tohoku-Oki earthquake and slow slip event revealed from seismic interferometry, using ocean bottom seismometer’s records"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317070234752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geological evidence for shallow ductile-brittle transition zones along subduction interfaces : example from the Shimanto Belt, SW Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792046945536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Along-strike variations in temperature and tectonic tremor activity along the Hikurangi subduction zone, New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996267021872768","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Possible large near-trench slip during the 2011 Mw 9.0 off the Pacific coast of Tohoku Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996267026808320","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"An estimate of tidal and non-tidal modulations of plate subduction speed in the transition zone in the Tokai district"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/j.tecto.2012.08.022"},{"@type":"KAKEN","@value":"PRODUCT-21340018"},{"@type":"KAKEN","@value":"PRODUCT-15313713"},{"@type":"KAKEN","@value":"PRODUCT-12506147"},{"@type":"KAKEN","@value":"PRODUCT-13679425"},{"@type":"KAKEN","@value":"PRODUCT-15313813"},{"@type":"OPENAIRE","@value":"doi_dedup___::05799ff515dfe853cc5a2d3d9d299961"},{"@type":"CROSSREF","@value":"10.1029/2019gl082817_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1002/2014gl061676_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1002/2017gl073460_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.20965/jdr.2014.p0317_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1002/2014gl059791_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1002/2016jb013417_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1002/2017gl072838_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1002/2017gl072876_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1029/2018gl080830_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1126/science.aaf2349_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1130/ges01531.1_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1186/s40623-014-0142-6_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1190/segj112013-117_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1029/2019jb017988_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1038/s41598-019-45781-0_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1126/science.aax5618_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1146/annurev-earth-060313-054614_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1785/0220180394_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1029/2020rg000713_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1029/2020jb020618_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1029/2020gl092173_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1038/s43017-020-00108-w_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1029/2021jb023336_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2022.229519_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1186/s40645-023-00556-0_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1186/s40623-025-02175-z_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2025.230763_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1029/2023jb027942_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.4116/jaqua.65.2507_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1002/2014gl062986_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1002/2015gl067569_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1007/s11001-013-9192-6_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1038/ngeo2547_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1126/science.aad3108_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1126/science.aaf1512_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.20965/jdr.2014.p0303_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.20965/jdr.2020.p0087_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1002/2017gl074307_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1002/2017jb014188_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1002/grl.50959_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1029/2018jb016651_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1186/s40623-014-0141-7_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1186/s40623-015-0311-2_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1186/s40623-017-0632-4_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.5194/sd-24-93-2018_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1016/j.jseaes.2016.07.011_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1029/2019gl084666_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1186/s40623-019-1076-9_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2020.116261_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1029/2020jb019613_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2020.228714_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1029/2020jb020284_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1186/s40623-021-01524-y_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.3389/feart.2021.744217_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2021.116742_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1103/physrevresearch.4.013211_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1016/j.enggeo.2022.106640_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2023.229845_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1029/2024jb029068_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1029/2024gl109384_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1007/s11001-013-9208-2_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1002/2015gl065829_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1029/2019gl082468_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1186/s40645-018-0240-3_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1785/0220180021_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2012.12.038_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1029/2020jb019527_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1038/s41467-020-14745-8_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1785/0220170173_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.2465/jmps.140403_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.4294/zisin.2016-18_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.3389/feart.2020.598270_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1093/gji/ggaa264_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1029/2021jb021706_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1029/2021jb023258_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1029/2020gc009329_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1186/s40623-023-01862-z_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1186/s40645-023-00579-7_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1029/2022jb024403_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1029/2023jb026457_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.21203/rs.3.rs-2604229/v1_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.21203/rs.3.rs-2040866/v1_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1029/2024gl110406_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1002/2016jb013391_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.20965/jdr.2014.p0311_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1002/2016jb013925_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1002/jgrb.50323_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1007/s00024-018-02089-w_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1029/2018jb015642_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1029/2018jb016072_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1093/gji/ggt424_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1186/s40645-018-0201-x_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2017.08.041_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2017.11.039_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1186/s40623-020-01212-3_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1093/gji/ggab331_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1146/annurev-earth-032320-074429_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1186/s40645-022-00526-y_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1038/s41598-022-16578-5_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2022.117443_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.3389/feart.2020.599810_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1007/s00024-022-03198-3_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1186/s40645-022-00528-w_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1029/2023jb027413_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1186/s40645-022-00523-1_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1029/2023gl104852_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.4294/zisin.2025-2s_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1029/2024jb030601_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1186/s40645-023-00575-x_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2024.230536_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1186/s40623-024-02004-9_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1093/gji/ggaf057_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.2183/pjab.89.391_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1146/annurev-earth-053018-060507_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.1186/s40623-019-1039-1_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.4294/zisin.69.1_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.5026/jgeography.126.207_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2017.0080_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.2183/pjab.96.022_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.2183/pjab.90.259_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"},{"@type":"CROSSREF","@value":"10.5363/tits.24.11_69_references_DOI_ZrVOPDrAvhz4OY9Rzr7DsdzftB7"}]}