{"@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/1390282679281133952.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.4294/zisin.66.15"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"024912305"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/024912305"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I024912305"}},{"identifier":{"@type":"NAID","@value":"10031202375"}}],"dc:title":[{"@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)"}],"dc:language":"ja","description":[{"type":"abstract","notation":[{"@language":"en","@value":"Long-term slow slip events occur adjacent to the seismogenic zones of major interplate earthquakes along the Nankai Trough in southwestern Japan. GNSS observations began about 20 years ago, but this is much shorter than the cycle of major interplate earthquakes. Knowing past long-term slow slips gives important information for understanding the preparation process of major earthquakes along the Nankai Trough. We extracted an unsteady component of vertical crustal deformations in the Kii Peninsula before GNSS deployment using leveling and sea-level data. GNSS-derived, steady-state vertical displacements related to ongoing subduction of the Philippine Sea Plate were subtracted from the vertical displacements observed by leveling surveys. Monthly mean sea-level data were corrected for atmospheric pressure and hydrographic effects. As a result, postseismic deformation of the 1944 Tonankai and the 1946 Nankai earthquakes was seen from 1972 to 1980. No unsteady component of vertical crustal deformation exceeding 3 cm was found from 1980 to 2009 in the Kii Peninsula. This means that a long-term slow slip event with at least more than moment magnitude (<I>M</I><SUB>w</SUB>) 6.5 may have not occurred in this period along the southeastern coast of the Kii Peninsula."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1410001204306713858","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000004601388"}],"foaf:name":[{"@language":"en","@value":"KOBAYASHI Akio"},{"@language":"ja","@value":"小林 昭夫"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Meteorological Research Institute"},{"@language":"ja","@value":"気象庁気象研究所"}]}],"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":"2013","prism:volume":"66","prism:number":"2","prism:startingPage":"15","prism:endingPage":"25"},"reviewed":"false","url":[{"@id":"http://id.ndl.go.jp/bib/024912305"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I024912305"}],"availableAt":"2013","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Vertical%20crustal%20deformation","dc:title":"Vertical crustal deformation"},{"@id":"https://cir.nii.ac.jp/all?q=Long-term%20slow%20slip","dc:title":"Long-term slow slip"},{"@id":"https://cir.nii.ac.jp/all?q=Leveling","dc:title":"Leveling"},{"@id":"https://cir.nii.ac.jp/all?q=Sea-level","dc:title":"Sea-level"},{"@id":"https://cir.nii.ac.jp/all?q=Kii%20Peninsula","dc:title":"Kii Peninsula"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360002216708861824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references","cites"],"jpcoar:relatedTitle":[{"@value":"3D modeling of the cycle of a great Tohoku-oki earthquake, considering frictional behavior at low to high slip velocities"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617909503360","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Crustal velocity field of southwest Japan: Subduction and arc‐arc collision"}]},{"@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/1360292619864898816","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Interseismic uplift at the Nankai subduction zone, southwest Japan, 1951–1990"}]},{"@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/1361699995792649856","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Source parameters and time‐dependent slip distributions of slow slip events on the Cascadia subduction zone from 1998 to 2008"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699996169205248","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Slow slip events controlled by the slab dip and its lateral change along a trench"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699996203426560","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Spatiotemporal distribution of interplate coupling in southwest Japan from inversion of geodetic data"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981470101059072","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Repetitive long-term slow slip events beneath the Bungo Channel, southwestern Japan, identified from leveling and sea level data from 1979 to 2008"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420329762688","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Detection of short‐term slow slip events along the Nankai Trough, southwest Japan, using GNSS data"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894457260416","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Detection and Monitoring of Ongoing Aseismic Slip in the Tokai Region, Central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825896132925568","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The earthquake deformation cycle at the Nankai Trough, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825896404139776","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Characteristics and interactions between non-volcanic tremor and related slow earthquakes in the Nankai subduction zone, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370858652416","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Seismic and geodetic evidence for the existence of hot materials beneath the Wakayama swarm activity, southwestern Japan"}]},{"@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/1363670320031417344","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Quasi‐periodic slow slip events in the afterslip area of the 1996 Hyuga‐nada earthquakes, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951793887664384","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Along‐strike variations in short‐term slow slip events in the southwest Japan subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204304382720","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@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)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204305438080","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"GPS連続観測による日本列島上下地殻変動とその意義"},{"@language":"en","@value":"Mapped Vertical Deformation Field of Japan Derived from Continuous GPS Measurements and Its Tectonic Implications"},{"@language":"ja-Kana","@value":"GPS レンゾク カンソク ニ ヨル ニホン レットウ ジョウゲ チカク ヘンドウ ト ソノ イギ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204307042304","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"地殻変動解析支援プログラムMICAP-Gの開発"},{"@language":"en","@value":"A Program to Assist Crustal Deformation Analysis"},{"@language":"ja-Kana","@value":"チカク ヘンドウ カイセキ シエン プログラム MICAP-G ノ カイハツ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679280336640","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Three-Dimensional Velocity Structure in Southwestern Japan and Configuration of the Philippine Sea Slab Estimated by Double-Difference Tomography"},{"@language":"ja","@value":"Double-Difference Tomography法による西南日本の3次元地震波速度構造およびフィリピン海プレートの形状の推定"},{"@language":"ja-Kana","@value":"Double Difference Tomographyホウ ニ ヨル セイナン ニホン ノ 3ジゲン ジシンハ ソクド コウゾウ オヨビ フィリピンカイ プレート ノ ケイジョウ ノ スイテイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681486404992","@type":"Article","relationType":["references","cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Co-seismic Displacements of the 1995 Hyogo-ken Nanbu Earthquake."},{"@language":"ja-Kana","@value":"Co-seismic Displacements of the 1995 Hy"}]},{"@id":"https://cir.nii.ac.jp/crid/1520009408858944512","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"東海地域の長期的スロースリップイベントおよび地震サイクルの再現の試み"},{"@language":"ja-Kana","@value":"トウカイ チイキ ノ チョウキテキ スロースリップイベント オヨビ ジシン サイクル ノ サイゲン ノ ココロミ"}]},{"@id":"https://cir.nii.ac.jp/crid/1520009409326585728","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"GPS連続観測システム(GEONET)解析結果に生じる人為的要因によるオフセットの補正手法について"},{"@language":"ja-Kana","@value":"GPS レンゾク カンソク システム GEONET カイセキ ケッカ ニ ショウジル ジンイテキ ヨウイン ニ ヨル オフセット ノ ホセイ シュホウ ニ ツイテ"}]},{"@id":"https://cir.nii.ac.jp/crid/1520290882024091264","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"測地測量が捉えた兵庫県南部地震に伴う地殻変動"},{"@language":"ja-Kana","@value":"ソクチ ソクリョウ ガ トラエタ ヒョウゴケン ナンブ ジシン ニ トモナウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1520290884125723392","@type":"Article","relationType":["cites"],"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/1520572358730069248","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"水準測量データから求めた日本列島100年間の地殻上下変動"},{"@language":"ja-Kana","@value":"スイジュン ソクリョウ データ カラ モトメタ ニホン レットウ 100ネンカン ノ チカク ジョウゲ ヘンドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1520572358917636992","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"GPS連続観測システム(GEONET)の新しい解析戦略(第4版)によるルーチン解析システムの構築について"},{"@language":"ja-Kana","@value":"GPS レンゾク カンソク システム GEONET ノ アタラシイ カイセキ センリャク ダイ4ハン ニ ヨル ルーチン カイセキ システム ノ コウチク ニ ツイテ"}]},{"@id":"https://cir.nii.ac.jp/crid/1520572358980784000","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"平均海面位変化と上下変動の検出に向けた験潮データの平滑化手法"},{"@language":"ja-Kana","@value":"ヘイキン カイメンイ ヘンカ ト ジョウゲ ヘンドウ ノ ケンシュツ ニ ムケタ ケンチョウ データ ノ ヘイカツカ シュホウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1520853832353436672","@type":"Article","relationType":["cites"],"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/1521699230934583552","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"潮位記録を用いた地殻上下変動推定のための津村による海域区分の検証"},{"@language":"ja-Kana","@value":"チョウイ キロク オ モチイタ チカク ジョウゲ ヘンドウ スイテイ ノ タメノ ツムラ ニ ヨル カイイキ クブン ノ ケンショウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1522543655564537856","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"Spatial and temporal evolution of the long-term slow slip in the Bungo Channel, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1570009749371810688","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"中部・近畿地方の上下変動"}]},{"@id":"https://cir.nii.ac.jp/crid/1570009749371812992","@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/1570291224348523136","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A variable span scatterplot smoother"}]},{"@id":"https://cir.nii.ac.jp/crid/1570572699325231360","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Crustal velocity field of southwest Japan: subduction and arc-arc collison"}]},{"@id":"https://cir.nii.ac.jp/crid/1570572699325232512","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Internal Deformation due to shear and Tensile Faults in a Half-space"}]},{"@id":"https://cir.nii.ac.jp/crid/1570572699325234944","@type":"Article","relationType":["cites"]},{"@id":"https://cir.nii.ac.jp/crid/1570854174301944576","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Quasi-periodic slow slip events in the afterslip area of the 1996 Hyuga-nada earthquakes, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1570854174301945728","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"平成23年度全国の地盤沈下地域の概況"}]},{"@id":"https://cir.nii.ac.jp/crid/1571135649278656128","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"日本沿岸の平均海面およびその変動の研究(I)-潮位変化の地域分布-"}]},{"@id":"https://cir.nii.ac.jp/crid/1571417124255361664","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"中部・近畿地方の上下変動"}]},{"@id":"https://cir.nii.ac.jp/crid/1571417124255363456","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Detection and monitoring of ongoing aseismic slip in the Tokai region, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1571417124255366784","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Characteristics and interctions between non-volcanic tremor and related slow earth-quales in the Nankai subduction zone, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1571417124255367936","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Seismic and geodetic evidence for the existence of hot materials beneath the Wakayama swarm activity, southwestern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1571980074208782848","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Along-strike variations in short-term slow slip events in the south-west Japan subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1571980074208785024","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Repetitive long-term slow slip events beneath the Bungo Channel, southwestern Japan, identified from leveling and sea level data from 1979 to 2008"}]},{"@id":"https://cir.nii.ac.jp/crid/1571980074208786176","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Spatiotemporal distribution of interplate coupling in southwest Japan from inversion of geodetic data"}]},{"@id":"https://cir.nii.ac.jp/crid/1571980074208787200","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"近畿地方の地殻変動"}]},{"@id":"https://cir.nii.ac.jp/crid/1572261549185495552","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"中部・近畿地方の上下変動"}]},{"@id":"https://cir.nii.ac.jp/crid/1572261549185496704","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"New, improved version of the Generic Mapping Tools releasae"}]},{"@id":"https://cir.nii.ac.jp/crid/1572824499138915968","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Slow slip events controlled by the slab sip and its lateral change along a trench"}]},{"@id":"https://cir.nii.ac.jp/crid/1572824499138917120","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"地殻変動解析支援プログラムの開発"}]},{"@id":"https://cir.nii.ac.jp/crid/1573387449092336128","@type":"Article","relationType":["cites"]},{"@id":"https://cir.nii.ac.jp/crid/1573387449092337408","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The earthquake deformation cycle at the Nankai trough, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1573387449092338432","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"電子基準点1200点の全国整備について"}]},{"@id":"https://cir.nii.ac.jp/crid/1573387449092340736","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Detection of short-term slow slip events along the Nankai Trough, southwest Japan, using GNSS data"}]},{"@id":"https://cir.nii.ac.jp/crid/1573950399045757696","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Interseismic uplift at the Nankai subduction zone, southwest Japan, 1951-1990"}]},{"@id":"https://cir.nii.ac.jp/crid/1573950399045758848","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"近畿地方の地殻変動"}]},{"@id":"https://cir.nii.ac.jp/crid/1573950399045761152","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"近畿地方の地殻変動"}]},{"@id":"https://cir.nii.ac.jp/crid/1573950399045762304","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Source parameters and time-dependent slip distributions of slow slip events on the Cascadia subduction zone from 1998 to 2008"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842091852032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Spatial and temporal evolution of the long-term slow slip in the Bungo Channel, Japan"}]}],"dataSourceIdentifier":[{"@type":"JALC","@value":"oai:japanlinkcenter.org:1002456717"},{"@type":"NDL_SEARCH","@value":"oai:ndlsearch.ndl.go.jp:R000000004-I024912305"},{"@type":"CROSSREF","@value":"10.4294/zisin.66.15"},{"@type":"CIA","@value":"10031202375"}]}