{"@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/1390001204304382720.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.4294/zisin.61.113"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"10267242"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/10267242"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I10267242"}},{"identifier":{"@type":"NAID","@value":"10024926476"}}],"dc:title":[{"@language":"en","@value":"Transient Crustal Deformation in the Tokai District"},{"@language":"ja","@value":"東海地方の非定常地殻変動"},{"@value":"東海地方の非定常地殻変動--東海スロースリップと2004年紀伊半島南東沖の地震の余効変動"},{"@language":"ja-Kana","@value":"トウカイ チホウ ノ ヒテイジョウ チカク ヘンドウ トウカイ スロースリップ ト 2004ネンキイハントウ ナントウオキ ノ ジシン ノ ヨコウヘンドウ"},{"@value":"Transient crustal deformation in the Tokai district: the Tokai slow slip event and postseismic deformation cause by the 2004 off southeast Kii Peninsula earthquake"},{"@value":"Transient crustal deformation in the Tokai district (in Japanese)"}],"dcterms:alternative":[{"@language":"en","@value":"—The Tokai Slow Slip Event and Postseismic Deformation Caused by the 2004 off Southeast Kii Peninsula Earthquake—"},{"@language":"ja","@value":"—東海スロースリップと2004年紀伊半島南東沖の地震の余効変動—"}],"dc:language":"ja","description":[{"type":"abstract","notation":[{"@language":"en","@value":"We investigated the transient crustal deformation in the Tokai district, central Japan, based on the GPS data in 2000-2008. Our modeling showed that observed transient deformation in the Tokai district can be explained by three different mechanisms, slow slip on the plate interface, viscoelastic response and an afterslip following the 2004 off southeast Kii peninsula earthquake. In our modeling, we first evaluated the effect of postseismic deformation due to the viscoelastic response of the 2004 off southeast Kii peninsula earthquake, and obtained the reasonable value of viscosity 1.0×10<SUP>19</SUP> Pa·s. Then we estimated the afterslip model of the 2004 off southeast Kii peninsula earthquake, and obtained that the time constant of the postseismic deformation caused by the afterslip is 62.65 days. After removing the viscoelastic response and the effect of afterslip from original transient deformation, we modeled this transient deformation as a slow slip on the plate interface, which we call here as Tokai slow slip event. Our result revealed that the Tokai slow slip which occurred mainly under the Lake Hamana ended in July 2005. The maximum slip of this event was estimated at 25cm under the Lake Hamana. This maximum slip accounts for the backslip accumulated in the past 14 years, assuming that the backslip rate has been constant. The total moment release was equivalent to that of an <I>M</I><SUB>w</SUB> 7.1 earthquake. On the other hand, the aseismic slip still continues in the northeast region of the Lake Hamana at the same rate as that before July 2005. The maximum slip in this region since July 2005 reaches 5cm, and total moment release is equivalent to that of an <I>M</I><SUB>w</SUB> 6.5 earthquake."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1410572172448577409","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000014231817"},{"@type":"NRID","@value":"9000014278345"},{"@type":"NRID","@value":"9000019210923"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0211155"}],"foaf:name":[{"@language":"en","@value":"SUITO Hisashi"},{"@language":"ja","@value":"水藤 尚"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Geography and Crustal Dynamics Research Center, Geographical Survey Institute of Japan"},{"@language":"ja","@value":"国土地理院地理地殻活動研究センター"}]},{"@id":"https://cir.nii.ac.jp/crid/1410572172448577408","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000014278346"}],"foaf:name":[{"@language":"en","@value":"OZAWA Shinzaburo"},{"@language":"ja","@value":"小沢 慎三郎"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Geography and Crustal Dynamics Research Center, Geographical Survey Institute of Japan"},{"@language":"ja","@value":"国土地理院地理地殻活動研究センター"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00371114"},{"@type":"LISSN","@value":"00371114"},{"@type":"EISSN","@value":"18839029"},{"@type":"EISSN","@value":"2186599X"},{"@type":"NDL_BIB_ID","@value":"000000009860"},{"@type":"ISSN","@value":"00371114"},{"@type":"NCID","@value":"AN00305741"}],"prism:publicationName":[{"@language":"en","@value":"Zisin (Journal of the Seismological Society of Japan. 2nd ser.)"},{"@language":"ja","@value":"地震　第２輯"},{"@value":"地震　第2輯"},{"@language":"ja","@value":"地震"},{"@language":"ja","@value":"地震　第２輯"},{"@language":"en","@value":"JSSJ"},{"@language":"en","@value":"Zisin"},{"@language":"en","@value":"BSSJ"},{"@language":"en","@value":"Zisin (Journal of the Seismological Society of Japan. 2nd ser.)"},{"@language":"en","@value":"Zisin1"},{"@language":"ja","@value":"地震１"},{"@language":"ja","@value":"地震　第１輯"}],"dc:publisher":[{"@language":"en","@value":"SEISMOLOGICAL SOCIETY OF JAPAN"},{"@language":"ja","@value":"公益社団法人 日本地震学会"}],"prism:publicationDate":"2009","prism:volume":"61","prism:number":"3","prism:startingPage":"113","prism:endingPage":"135"},"reviewed":"false","url":[{"@id":"http://id.ndl.go.jp/bib/10267242"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I10267242"}],"availableAt":"2009","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Tokai%20slow%20slip","dc:title":"Tokai slow slip"},{"@id":"https://cir.nii.ac.jp/all?q=Postseismic%20deformation","dc:title":"Postseismic deformation"},{"@id":"https://cir.nii.ac.jp/all?q=Afterslip","dc:title":"Afterslip"},{"@id":"https://cir.nii.ac.jp/all?q=Viscoelastic%20response","dc:title":"Viscoelastic response"},{"@id":"https://cir.nii.ac.jp/all?q=2004%20off%20southeast%20Kii%20peninsula%20earthquake","dc:title":"2004 off southeast Kii peninsula earthquake"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001202062872704","@type":"Article","resourceType":"紀要論文(departmental bulletin paper)","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"西南日本外帯における地殻下地震の活動特性"},{"@language":"en","@value":"Characteristic Activities of Subcrustal Earthquakes along the Outer Zone of Southwestern Japan"},{"@language":"ja-Kana","@value":"セイナン ニホンガイタイ ニ オケル チカクカ ジシン ノ カツドウ トクセイ"}]},{"@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/1050585172435286656","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Spatiotemporal changes in the strain field in the Niigata–Kobe Tectonic Zone: long-term analysis using GNSS time series data"}]},{"@id":"https://cir.nii.ac.jp/crid/1050859447951740800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Strain accumulation and release associated with the occurrence of SSEs in the subduction zones of the Japanese Islands"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011143604403328","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Post-earthquake ground movements correlated to pore-pressure transients"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011146029635072","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Short‐term slow slip and correlated tremor episodes in the Tokai region, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168721764352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Role of Fluid‐Related Heterogeneous Structures in Controlling the Fault Slip Behavior in the Slow‐Earthquake Source Region Along the Nankai Subduction Zone, Southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017279827067392","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A combination of tides and nontidal variations in ocean bottom pressure may generate interannual slip fluctuations in the transition zone along a subduction plate interface"}]},{"@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/1360292617909532032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"New, improved version of generic mapping tools released"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617916830848","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Source mechanisms and tectonic significance of historical earthquakes along the nankai trough, Japan"}]},{"@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/1360572092857193856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Variations in the Characteristic Amplitude of Tectonic Tremor Induced by Long‐Term Slow Slip Events"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574094253735680","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Co‐seismic slip, post‐seismic slip, and largest aftershock associated with the 1994 Sanriku‐haruka‐oki, Japan, earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846641638535936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dynamic modeling of slow slip coupled with tremor"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848658222185728","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Slip‐Deficit Rate Distribution Along the Nankai Trough, Southwest Japan, With Elastic Lithosphere and Viscoelastic Asthenosphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570591305088","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Spatial and temporal evolution of stress and slip rate during the 2000 Tokai slow earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855571518041600","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Interplate coupling and relative plate motion in the Tokai district, central Japan, deduced from geodetic data inversion using ABIC"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137046325353216","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Interplate coupling in the Tokai District, central Japan, deduced from continuous GPS data"}]},{"@id":"https://cir.nii.ac.jp/crid/1361412893057002880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatiotemporal Evolution of Long‐ and Short‐Term Slow Slip Events in the Tokai Region, Central Japan, Estimated From a Very Dense GNSS Network During 2013–2016"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994539372672","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Occurrence of quasi-periodic slow-slip off the east coast of the Boso peninsula, Central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994628373632","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Aseismic slip and low‐frequency earthquakes in the Bungo channel, southwestern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262944428006784","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Characteristic silent earthquakes in the eastern part of the Boso peninsula, Central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262944447488896","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Lithospheric loading by the 1896 Riku‐u Earthquake, northern Japan: Implications for plate flexure and asthenospheric rheology"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420986062464","@type":"Article","relationType":["cites"],"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/1362825894457260416","@type":"Article","relationType":["references","cites"],"jpcoar:relatedTitle":[{"@value":"Detection and Monitoring of Ongoing Aseismic Slip in the Tokai Region, Central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370689065856","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Distribution of seismic coupling on the subducting plate boundary in northeastern Japan inferred from GPS observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370884162816","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Slow slip transients along the Oaxaca subduction segment from 1993 to 2007"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370931521408","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Lithospheric rheology in southern Italy inferred from postseismic viscoelastic relaxation following the 1980 Irpinia earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388843526550272","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A slow thrust slip event following the two 1996 Hyuganada Earthquakes beneath the Bungo Channel, southwest Japan"}]},{"@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/1363388844894824320","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Observation of coseismic seafloor crustal deformation due to <i>M</i>7 class offshore earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388846161768960","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Partitioning between seismogenic and aseismic slip as highlighted from slow slip events in Hyuga‐nada, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670319089972224","@type":"Article","relationType":["references","cites"],"jpcoar:relatedTitle":[{"@value":"Silent fault slip following an interplate thrust earthquake at the Japan Trench"}]},{"@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/1363951796156178048","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Parallel simulation system for earthquake generation: fault analysis modules and parallel coupling analysis"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233268603254528","@type":"Article","relationType":["references","cites"],"jpcoar:relatedTitle":[{"@value":"Time‐dependent inversion study of the slow thrust event in the Nankai trough subduction zone, southwestern Japan"}]},{"@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/1364233271032329216","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Reexamination of the interplate coupling in the Tokai region, central Japan, based on the GPS data in 1997–2002"}]},{"@id":"https://cir.nii.ac.jp/crid/1370002220375126026","@type":"Product","relationType":["references"]},{"@id":"https://cir.nii.ac.jp/crid/1370288171517519115","@type":"Product","relationType":["references"]},{"@id":"https://cir.nii.ac.jp/crid/1370288171801073672","@type":"Product","relationType":["references"]},{"@id":"https://cir.nii.ac.jp/crid/1370851121823968646","@type":"Product","relationType":["references"]},{"@id":"https://cir.nii.ac.jp/crid/1371975295158667534","@type":"Product","relationType":["references"]},{"@id":"https://cir.nii.ac.jp/crid/1390001204303147776","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"季節変動を補正した水準測量データに基づく東海地域の最近の地殻変動"},{"@language":"en","@value":"Recent Crustal Movement in the Tokai Area, Japan As Inferred from the Seasonal Effect Corrected Levelling Data"},{"@language":"ja-Kana","@value":"キセツ ヘンドウ オ ホセイシタ スイジュン ソクリョウ データ ニ モトズク"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204306976896","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"1989年12月東京湾サイレント・アースクェイクの可能性"},{"@language":"en","@value":"A Silent Earthquake of December 9, 1989, in the Tokyo Bay, as Revealed by the Continuous Observation of Crustal Movements in the Southern Kanto District, Central Japan"},{"@language":"ja-Kana","@value":"1989ネン 12ガツ トウキョウワン サイレント アースクェイク ノ カノウセイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206509222144","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Study of periodic vertical crustal movement in the Omaezaki peninsula, Central Japan, and it's tectonic implications"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206511385984","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The 1992 Sanriku-Oki, Japan, Ultra-Slow Earthquake."}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206511842048","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Coseismic and postseismic crustal deformation after the M<SUB>ω</SUB> 8 Tokachi-oki earthquake in Japan"},{"@value":"Coseismic and postseismic crustal deformation after the Mw 8 Tokachi-oki earthquake in Japan"},{"@value":"Post seismic crustal deformation from the Mw 8 Tokachi-oki earthquake on September 26, 2003 in Japan"},{"@value":"Co-seismic and post-seismic crustal deformation after the M8 Tokachi-oki earthquake in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206513093632","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Transient crustal deformation in Tokai region, central Japan, until May 2004"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206513406976","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Source rupture processes of the 1944 Tonankai earthquake and the 1945 Mikawa earthquake derived from low-gain seismograms"},{"@value":"Source rupture process of the 1944 Tonankai earthquake and the 1945 Mikawa earthquake derived from low‐gain seismograms"},{"@value":"Source rupture process of the 1944 Tonankai earthquake and the 1945 Mikawa earthquake derived from low-gain seismograms"}]},{"@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/1390282679280495104","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Long-term Slow Slip Event around Kochi City from 1977 to 1980"},{"@language":"ja","@value":"高知市付近で１９７７～１９８０年頃に発生した長期的スロースリップ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679280669184","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Source Mechanism of an Intraslab Earthquake in thePhilippine Sea Plate; the <I>M</I>5.6 Earthquake under Eastern Mino, Gifu Prefecture, Japan"},{"@language":"ja","@value":"フィリピン海プレート内で発生した岐阜県美濃東部の地震 (<I>M</I>5.6) の発生メカニズム"},{"@value":"フィリピン海プレート内で発生した岐阜県美濃東部の地震(M5.6)の発生メカニズム"},{"@language":"ja-Kana","@value":"フィリピンカイ プレート ナイ デ ハッセイ シタ ギフケン ミノ トウブ ノ ジシン(M5.6)ノ ハッセイ メカニズム"},{"@value":"Source Mechanism of an Intraslab Earthquake in thePhilippine Sea Plate; the M5.6 Earthquake under Eastern Mino, Gifu Prefecture, Japan"},{"@value":"Source mechanism of an intraslab earthquake in the Philippine Sea plate: the M5.6 earthquake under eastern Mono, Gifu prefecture, Japan (in Japanese with English abstract)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679280956544","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A Small Scale Long-term Slow Slip Occurred in the Western Shikoku in 2005"},{"@value":"四国西部において2005年に発生した小規模な長期的スロースリップ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679281133952","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Vertical Crustal Deformation in the Kii Peninsula Deduced from Leveling and Sea-Level Data, 1972-2009"},{"@language":"ja","@value":"水準測量と潮位による紀伊半島の地殻上下変動（1972～2009年）"},{"@language":"ja-Kana","@value":"スイジュン ソクリョウ ト チョウイ ニ ヨル キイ ハントウ ノ チカク ジョウゲ ヘンドウ(1972~2009ネン)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679281457024","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Short-term Slow Slip Events Detected by the Strainmeters in Tokai Region in the Period from 1984 to 2005"},{"@language":"ja","@value":"歪計により観測された東海地域の短期的スロースリップ（1984～2005年）"},{"@language":"ja-Kana","@value":"ヒズミケイ ニ ヨリ カンソク サレタ トウカイ チイキ ノ タンキテキ スロースリップ 1984 2005ネン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679283912192","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"東海地域のフィリピン海スラブ形状と収束テクトニクス"},{"@language":"en","@value":"Geometry of the Philippine Sea Slab and the Convergent Tectonics in the Tokai District, Japan"},{"@language":"ja-Kana","@value":"トウカイ チイキ ノ フィリピンカイ スラブ ケイジョウ ト シュウソク テク"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681216800384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Average recurrence interval of Ansei-type earthquakes inferred from Holocene deposits of the Yaizu Plain, Shizuoka Prefecture, Japan"},{"@language":"ja","@value":"静岡県焼津平野の完新統の解析に基づく安政型地震の平均発生間隔の推定"},{"@language":"ja-Kana","@value":"シズオカケン ヤイズ ヘイヤ ノ カンシントウ ノ カイセキ ニ モトズク アンセイガタ ジシン ノ ヘイキン ハッセイ カンカク ノ スイテイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681217064448","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Crustal deformation of northeastern Japan based on geodetic data for recent 120 years"},{"@language":"ja","@value":"測地観測データに基づく東北日本の最近120年間の地殻変動"},{"@language":"ja-Kana","@value":"ソクチ カンソク データ ニ モトズク トウホク ニホン ノ サイキン 120ネンカン ノ チカク ヘンドウ"},{"@value":"Crustal deformation of northeastern Japan based on geodetic data for recent 120 years [in Japanese with English abstract]"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681488592896","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Seafloor displacement at Kumano-nada caused by the 2004 off Kii Peninsula earthquakes, detected through repeated GPS/Acoustic surveys"},{"@value":"Seafloor displacement at Kumano‐nada caused by the 2004 off Kii Peninsula earthquakes, detected through repeated GPS/Acoustic surveys"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489272064","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Urgent aftershock observation of the 2004 off the Kii Peninsula earthquake using ocean bottom seismometers"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489274368","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Spatial distribution of centroid moment tensor solutions for the 2004 off Kii peninsula earthquakes"},{"@value":"Spatial distribution of centroid moment tensor solutions for the 2004 off Kii peninsula earthquakes: a dynamic deformation process in the large accretionary prism"}]},{"@id":"https://cir.nii.ac.jp/crid/1391694356260521728","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Application of an Objective Detection Method of Long-Term Slow Slip Events using GNSS Data: Detection of Short-Term Slow Slip Events and Estimation of Moment Magnitude of Long-Term Slow Slip Events"},{"@language":"ja","@value":"GNSSによる長期的スロースリップ客観検出手法の応用―短期的スロースリップの検出と長期的スロースリップの規模推定―"}]},{"@id":"https://cir.nii.ac.jp/crid/1520009407400318464","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@value":"地殻変動検出のためのスタッキング手法の開発 : 東海地域のひずみ計データによるプレート境界すべり早期検知への適用"},{"@language":"ja-Kana","@value":"チカク ヘンドウ ケンシュツ ノ タメ ノ スタッキング シュホウ ノ カイハツ : トウカイ チイキ ノ ヒズミ ケイ データ ニ ヨル プレート キョウカイスベリ ソウキ ケンチ エ ノ テキヨウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1520009408761375232","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"舞阪の潮位変化から推定される東海スロースリップの繰り返し発生"},{"@language":"ja-Kana","@value":"マイサカ ノ チョウイ ヘンカ カラ スイテイ サレル トウカイ スロースリップ ノ クリカエシ ハッセイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1520009410241625216","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"南関東・東海地方の地殻活動の相互関連--フイリッピン海プレート北縁の最近の地殻ダイナミックス"},{"@language":"ja-Kana","@value":"ミナミ カントウ トウカイ チホウ ノ チカク カツドウ ノ ソウゴ カンレン"}]},{"@id":"https://cir.nii.ac.jp/crid/1520290882441289984","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"小特集:電子基準点1,200点の全国整備について"},{"@language":"ja-Kana","@value":"ショウトクシュウ デンシ キジュンテン 1 200テン ノ ゼンコク セイビ ニ ツイテ"}]},{"@id":"https://cir.nii.ac.jp/crid/1520290884125723392","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@value":"高知市付近で1977~1980年頃に発生した長期的スロースリップ"},{"@language":"ja-Kana","@value":"コウチシ フキン デ 1977~1980ネン ゴロ ニ ハッセイ シタ チョウキテキ スロースリップ"}]},{"@id":"https://cir.nii.ac.jp/crid/1520572358074730496","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"総合報告 2004年9月5日に紀伊半島沖・東海道沖で発生した地震の活動概要"},{"@language":"ja-Kana","@value":"ソウゴウ ホウコク 2004ネン 9ガツ 5ニチ ニ キイハントウオキ トウカイドウオキ デ ハッセイ シタ ジシン ノ カツドウ ガイヨウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1520572360190256128","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"日本の最近の地殻の水平変動と地震活動との関係-1-〔英文〕"},{"@language":"ja-Kana","@value":"ニホン ノ サイキン ノ チカク ノ スイヘイ ヘンドウ ト ジシン カツドウ ト ノ カンケイ 1 エイブン"}]},{"@id":"https://cir.nii.ac.jp/crid/1520853832353436672","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@value":"四国西部において2005年に発生した小規模な長期的スロースリップ"},{"@language":"ja-Kana","@value":"シコク セイブ ニ オイテ 2005ネン ニ ハッセイ シタ ショウキボ ナ チョウキテキ スロースリップ"}]},{"@id":"https://cir.nii.ac.jp/crid/1520853833517621504","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"地殻活動観測データ総合解析システムの開発"},{"@language":"ja-Kana","@value":"チカク カツドウ カンソク データ ソウゴウ カイセキ システム ノ カイハツ"}]},{"@id":"https://cir.nii.ac.jp/crid/1521699231017509376","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"1980年代における東海地方の異常歪変化"},{"@language":"ja-Kana","@value":"1980ネンダイ ニ オケル トウカイ チホウ ノ イジョウ ヒズミ ヘンカ"}]},{"@id":"https://cir.nii.ac.jp/crid/1522543654797847424","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"Occurrence of quasi-periodic slow-slip off the east coast of the Boso peninsula, Central Japan"},{"@language":"ja-Kana","@value":"Occurrence of quasi periodic slow slip off the east coast of the Boso peninsula Central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1570009749568789376","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The 1992 Sanriku-Oki, Japan, Ultra-Slow Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1570291225782304128","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Slow slip events at the Alaska Subduction Zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1570291226740173056","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Interplate coupling and relative plate motion in the Tokai district, central Japan, deduced from geodetic data inversion using ABIC"}]},{"@id":"https://cir.nii.ac.jp/crid/1570572701504927616","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Lithospheric loading by the 1896 Riku-u earthquake, northern Japan : Implications for plate flexure and asthenospheric rheology"}]},{"@id":"https://cir.nii.ac.jp/crid/1570854175735727104","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Irpinia earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1571135650812714624","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"GPS observations of postseismic deformation for the 1995 Hyogo-ken Nanbu earthquake, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1571135651719241984","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Interplate coupling in the Tokai district, central Japan, deduced from continuous GPS data"}]},{"@id":"https://cir.nii.ac.jp/crid/1571417125689767680","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Repeated occurrence of slow slip events on the subducting plate interface in the Tokai region, central Japan, the focal region of the anticipated Tokai earthquake (M=8.0)"}]},{"@id":"https://cir.nii.ac.jp/crid/1571417125785088768","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Time dependent inversion of geodetic data"}]},{"@id":"https://cir.nii.ac.jp/crid/1571417126686954368","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A slow thrust slip event following the two 1996 Hyuganada earthquakes beneath the Bungo Channel, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1571698599993787776","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A silent slip event on the deeper Cascadia subduction interface"}]},{"@id":"https://cir.nii.ac.jp/crid/1571698600665856256","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"東海地震に関する専門調査会報告の概要"}]},{"@id":"https://cir.nii.ac.jp/crid/1571698600666483712","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@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/1572261549951338624","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Postglacial rebound at the northern Cascadia subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1572261550619900672","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"中部 近畿地方の地殻変動"}]},{"@id":"https://cir.nii.ac.jp/crid/1572261550619902976","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Reexamination of the interplate coupling in the Tokai region, central Japan, based on the GPS data in 1997-2002"}]},{"@id":"https://cir.nii.ac.jp/crid/1572261551571767936","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"On the mechanics of earthquake afterslip"}]},{"@id":"https://cir.nii.ac.jp/crid/1572543025595990144","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Parallel simulation system for earthquake generation : Fault analysis modules and parallel coupling analysis, Concurrency Computat"}]},{"@id":"https://cir.nii.ac.jp/crid/1572543025596613760","@type":"Article","relationType":["cites"]},{"@id":"https://cir.nii.ac.jp/crid/1572543026603388928","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Distribution of seismic coupling on the subducting plate boundary in northeastern Japan inferred from GPS observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1572824499340632064","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Simulated Empirical Law of Coseismic Crustal Deformation"}]},{"@id":"https://cir.nii.ac.jp/crid/1572824500572700288","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Slow slip transients along the Oaxaca subduction segment from 1993 to 2007"}]},{"@id":"https://cir.nii.ac.jp/crid/1572824500572702720","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"西南日本の深部低周波微動に同期する短期的スロースリップイベント (2004年11月-12月)"}]},{"@id":"https://cir.nii.ac.jp/crid/1572824501537370368","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Postseismic deformation following the Landers earthquake, California, 28 June 1992"}]},{"@id":"https://cir.nii.ac.jp/crid/1572824501565571328","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Poroelastic rebound along the Landers 1992 earthquake surface rupture"}]},{"@id":"https://cir.nii.ac.jp/crid/1573387450526743936","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"南アラスカで発生する時定数の異なるスロースリップイベント"}]},{"@id":"https://cir.nii.ac.jp/crid/1573387450526745728","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"2004年9月5日紀伊半島南東沖で発生した地震について"}]},{"@id":"https://cir.nii.ac.jp/crid/1573387450526747008","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"New improved version of the Generic Mapping Tools released"}]},{"@id":"https://cir.nii.ac.jp/crid/1573387451530309120","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Effects of three-dimensional inhomogeneous viscoelastic structures on post-seismic surface deformations associated with the great 1946 Nankaido earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1573387451533874048","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Simulation of postseismic deformation caused by the 1896 Riku-u earthquake, northeast Japan : Re-evaluation of the viscosity in the upper mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1573387451550645376","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Post-earthquake ground movements correlated to pore-pressure transients"}]},{"@id":"https://cir.nii.ac.jp/crid/1573387451550862848","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Co-seismic slip, postseismic slip, and largest aftershock associated with the 1994 Sanriku-haruka-oki, Japan, earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1573668925163719552","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"2004年紀伊半島南東沖地震震源域の地殻構造と余震分布について"},{"@language":"en","@value":"Crustal Structure and Urgent Aftershock Observation of the 2004 Off Kii-Peninsula Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1573668925503454592","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Observation of coseismic seafloor crustal deformation due to M 7 class offshore earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1573668925503457792","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"9月5日の紀伊半島南東沖地震 (本震 : M_j7.4) の再解析, EIC地震学ノート, 153"}]},{"@id":"https://cir.nii.ac.jp/crid/1573950399812084608","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Transient slip on the subduction interface in Guerrero, southern Mexico"}]},{"@id":"https://cir.nii.ac.jp/crid/1573950400479542272","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"上野巳新田-富巻山間の距離変化"}]},{"@id":"https://cir.nii.ac.jp/crid/1573950400479544448","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Slow slip on the northern Hikurangi subduction interface, New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1573950400480164224","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Characteristic silent earthquakes in the eastern part of the Boso peninsula, Central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1573950400480165376","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A large slow slip event and the depth of the seismogenic zone in the south central Alaska subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1573950400480168960","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Aseismic slip and low-frequency earthquakes in the Bungo channel, southwestern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1573950401231165824","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Source mechanisms and tectonic significance of historical earthquakes along the Nankai trough, Japan."}]},{"@id":"https://cir.nii.ac.jp/crid/1573950401491086720","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Partitioning between seismogenic and aseismic slip as highlighted from slow slip events in Hyuga-nada, Japan"},{"@value":"Partitioning between seismogenic and aseismic slip as highlighted from slow slip events in Hyuga‐nada, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1574231873792667776","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A simple and efficient method for introducing faults into finite element computations"}]},{"@id":"https://cir.nii.ac.jp/crid/1574231875456254080","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"東海地方に予想される大地震の再検討-駿河湾大地震について-"}]},{"@id":"https://cir.nii.ac.jp/crid/1574231875456255232","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Short-term slow slip and correlated tremor episodes in the Tokai region, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1574231875456875904","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Spatial and temporal evolution of stress and slip rate during the 2000 Tokai slow earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1574231875456878080","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Slow slip events and seismic tremor at circum-Pacific subduction zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1574231875456879232","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Space time distribution of afterslip following the 2003 Tokachi-oki earthquake : Implications for variations in fault zone frictional properties"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151841914167808","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Two long-term slow slip events around Tokyo Bay found by GNSS observation during 1996-2011"}]},{"@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":"JALC","@value":"oai:japanlinkcenter.org:0033068139"},{"@type":"NDL_SEARCH","@value":"oai:ndlsearch.ndl.go.jp:R000000004-I10267242"},{"@type":"CROSSREF","@value":"10.4294/zisin.61.113"},{"@type":"CIA","@value":"10024926476"},{"@type":"CROSSREF","@value":"10.20965/jdr.2014.p0317_references_DOI_QaJj417WCd95SGSUuGJssGiMdDD"},{"@type":"CROSSREF","@value":"10.1146/annurev-earth-060313-054614_references_DOI_QaJj417WCd95SGSUuGJssGiMdDD"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2016.0022_references_DOI_QaJj417WCd95SGSUuGJssGiMdDD"},{"@type":"CROSSREF","@value":"10.1029/2020gl089882_references_DOI_QaJj417WCd95SGSUuGJssGiMdDD"},{"@type":"CROSSREF","@value":"10.1029/2019jb018650_references_DOI_QaJj417WCd95SGSUuGJssGiMdDD"},{"@type":"CROSSREF","@value":"10.2467/mripapers.69.1_references_DOI_QaJj417WCd95SGSUuGJssGiMdDD"},{"@type":"CROSSREF","@value":"10.1016/j.geog.2022.09.001_references_DOI_QaJj417WCd95SGSUuGJssGiMdDD"},{"@type":"CROSSREF","@value":"10.1186/s40623-024-02009-4_references_DOI_QaJj417WCd95SGSUuGJssGiMdDD"},{"@type":"CROSSREF","@value":"10.1126/science.aaf1512_references_DOI_QaJj417WCd95SGSUuGJssGiMdDD"},{"@type":"CROSSREF","@value":"10.1186/s40623-015-0311-2_references_DOI_QaJj417WCd95SGSUuGJssGiMdDD"},{"@type":"CROSSREF","@value":"10.1186/s40623-017-0628-0_references_DOI_QaJj417WCd95SGSUuGJssGiMdDD"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2012.0027_references_DOI_QaJj417WCd95SGSUuGJssGiMdDD"},{"@type":"CROSSREF","@value":"10.4294/zisin.64.63_references_DOI_QaJj417WCd95SGSUuGJssGiMdDD"},{"@type":"CROSSREF","@value":"10.4294/zisin.63.97_references_DOI_QaJj417WCd95SGSUuGJssGiMdDD"},{"@type":"CROSSREF","@value":"10.1038/s41598-023-28016-1_references_DOI_QaJj417WCd95SGSUuGJssGiMdDD"},{"@type":"CROSSREF","@value":"10.1029/2010jb008136_references_DOI_QaJj417WCd95SGSUuGJssGiMdDD"},{"@type":"CROSSREF","@value":"10.1029/2018jb015515_references_DOI_QaJj417WCd95SGSUuGJssGiMdDD"},{"@type":"CROSSREF","@value":"10.1029/2020jb021138_references_DOI_QaJj417WCd95SGSUuGJssGiMdDD"},{"@type":"CROSSREF","@value":"10.1186/s40645-025-00688-5_references_DOI_QaJj417WCd95SGSUuGJssGiMdDD"}]}