{"@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/1362262944863495680.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1111/j.1365-246x.2008.03786.x"}},{"identifier":{"@type":"URI","@value":"http://academic.oup.com/gji/article-pdf/173/3/1018/5892484/173-3-1018.pdf"}}],"dc:title":[{"@value":"Simple relationship between seismic activity along Philippine Sea slab and geometry of oceanic Moho beneath southwest Japan"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382262944863495681","@type":"Researcher","foaf:name":[{"@value":"Katsuhiko Shiomi"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262944863495680","@type":"Researcher","foaf:name":[{"@value":"Makoto Matsubara"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262944863495682","@type":"Researcher","foaf:name":[{"@value":"Yoshihiro Ito"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262944863495683","@type":"Researcher","foaf:name":[{"@value":"Kazushige Obara"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"0956540X"},{"@type":"EISSN","@value":"1365246X"}],"prism:publicationName":[{"@value":"Geophysical Journal International"}],"dc:publisher":[{"@value":"Oxford University Press (OUP)"}],"prism:publicationDate":"2008-06","prism:volume":"173","prism:number":"3","prism:startingPage":"1018","prism:endingPage":"1029"},"reviewed":"false","url":[{"@id":"http://academic.oup.com/gji/article-pdf/173/3/1018/5892484/173-3-1018.pdf"}],"createdAt":"2008-04-24","modifiedAt":"2023-05-17","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050012570393434752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Three‐dimensional numerical modeling of temperature and mantle flow fields associated with subduction of the Philippine Sea plate, southwest Japan"},{"@value":"Three-dimensional numerical modeling of temperature and mantle flow fields associated with subduction of the Philippine Sea plate, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1050845763140670720","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Estimate of the contraction rate of central Japan through the deformation of the Philippine Sea slab"}]},{"@id":"https://cir.nii.ac.jp/crid/1050855511197307776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Seismological Structures on Bimodal Distribution of Deep Tectonic Tremor"}]},{"@id":"https://cir.nii.ac.jp/crid/1050856995322335104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Slip Distributions of Short-Term Slow Slip Events in Shikoku, Southwest Japan, From 2001 to 2019 Based on Tilt Change Measurements"},{"@value":"Slip Distributions of Short‐Term Slow Slip Events in Shikoku, Southwest Japan, From 2001 to 2019 Based on Tilt Change Measurements"}]},{"@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/1360002215916314624","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Identification of the static backstop and its influence on the evolution of the accretionary prism in the Nankai Trough"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216708861824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"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/1360004229808521216","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Resolving the Detailed Spatiotemporal Slip Evolution of Deep Tremor in Western Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232425569408","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Upper boundary of the Pacific plate subducting beneath Hokkaido, Japan, estimated from ScSp phase"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168722329344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismological evidence of a dehydration reaction in the subducting oceanic crust beneath western Shikoku in southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704781198720","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismic attenuation structure associated with episodic tremor and slip zone beneath Shikoku and the Kii peninsula, southwestern Japan, in the Nankai subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707402276864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"3D upper mantle structure beneath Japan and its surrounding region from inter-station dispersion measurements of surface waves"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707500223104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Slow slip rate and excitation efficiency of deep low-frequency tremors beneath southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165846900352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A systematic review of geological evidence for Holocene earthquakes and tsunamis along the Nankai-Suruga Trough, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179757877120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Hydrous state of the subducting Philippine Sea plate inferred from receiver function image using onshore and offshore data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182476844800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The weakened lower crust beneath the Nobi fault system, Japan: Implications for stress accumulation to the seismogenic zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182476923136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Receiver function images of the distorted Philippine Sea slab contact with the continental crust: Implications for generation of the 1891 Nobi earthquake (Mj 8.0)"}]},{"@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/1360584339753569536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Anisotropic Velocity Structure Beneath Shikoku, Japan: Insights From Receiver Function and Shear Wave Splitting Analyses"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848654732539648","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"<i>S</i> wave attenuation structure on the western side of the Nankai subduction zone: Implications for fluid distribution and dynamics"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657065501312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Two types of antigorite serpentinite controlling heterogeneous slow-slip behaviours of slab–mantle interface"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861705578184576","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Complex Interaction, Striations, and Periodicity of Deep Tremor Surrounding a Tremor Gap in the Central Nankai Subduction Zone, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204303053440","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Discovery of Slow Earthquake Families Associated with the Subduction of the Philippine Sea Plate in Southwest Japan"},{"@language":"ja","@value":"フィリピン海プレート沈み込みに伴う西南日本のスロー地震群の発見"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205082427008","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"島根県津和野地域に分布する高塩濃度地下水の地球化学的特徴と湧出機構"},{"@language":"en","@value":"Geochemical features and the flow system for saline mineral spring at the Tsuwano Town, Shimane Prefecture"},{"@language":"ja-Kana","@value":"シマネケン ツワノ チイキ ニ ブンプ スル コウエン ノウド チカスイ ノ チキュウ カガクテキ トクチョウ ト ユウシュツ キコウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205532988416","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"深部微動が明らかにする潮汐のプレート運動への影響"},{"@language":"en","@value":"Controls on plate motion by oscillating tidal stress: Evidence from deep tremors in western Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206237224448","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Shallow, deep slow earthquake families associated with the subduction of the Philippine Sea plate"},{"@language":"ja","@value":"フィリピン海プレート沈み込みに伴う浅部および深部スロー地震群"},{"@language":"ja-Kana","@value":"フィリピンカイ プレート シズミ コミ ニ トモナウ センブ オヨビ シンブ スロー ジシングン"}]},{"@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/1390282679206691072","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Detecting of the Moho Discontinuities Using Seismological Surveys: A Case in the Kinki District"},{"@language":"ja","@value":"地震学的探査によるモホ不連続面の検出―近畿地方を例として―"},{"@language":"ja-Kana","@value":"ジシンガクテキ タンサ ニ ヨル モホ フレンゾクメン ノ ケンシュツ キンキ チホウ オ レイ ト シテ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679280762880","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Crustal Structure in the Japanese Islands Inferred from Receiver Function Analysis"},{"@value":"レシーバ関数解析から推定された日本列島の地殻構造"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679281126528","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Construction of NIED High Sensitivity Seismograph Network (Hi-net) and its Contribution"},{"@language":"ja","@value":"防災科研 Hi-net の構築とその成果"},{"@language":"ja-Kana","@value":"ボウサイカケン Hi net ノ コウチク ト ソノ セイカ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282763073517952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"水平動地震計特性の違いが地下構造推定に与える影響"},{"@language":"en","@value":"Effect on the Subsurface Structure Estimation by the Difference in Responses of Two Horizontal Component Seismographs"},{"@language":"ja-Kana","@value":"スイヘイドウ ジシンケイ トクセイ ノ チガイ ガ チカ コウゾウ スイテイ ニ アタエル エイキョウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390564238076151040","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"地震波解析と波動伝播計算に基づく地球内部の短波長不均質構造の研究"},{"@language":"en","@value":"Study of Small-scale Heterogeneities in the Earth Inferredfrom Analysis of Observed and Simulated Seismograms"},{"@language":"ja-Kana","@value":"ジシンハ カイセキ ト ハドウ デンパ ケイサン ニ モトズク チキュウ ナイブ ノ タンハチョウ フキンシツ コウゾウ ノ ケンキュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714791869783424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dissimilar receiver functions observed at very close stations in the Kii Peninsula, central Japan : features and causes"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792046931712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Application of cluster analysis based on waveform cross-correlation coefficients to data recorded by ocean-bottom seismometers : results from off the Kii Peninsula"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1111/j.1365-246x.2008.03786.x"},{"@type":"CROSSREF","@value":"10.20965/jdr.2014.p0317_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.1002/2017jb014494_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.5026/jgeography.117.45_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2015.09.011_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.1093/gji/ggaa423_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.1029/2020gl092183_references_DOI_CC3rgNCIczR6iCN16iCE4iC4uIn"},{"@type":"CROSSREF","@value":"10.1002/2014gl060035_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.1002/2016jb012912_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.1002/2015jb012493_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.1186/1880-5981-66-80_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.4294/zisin.61.315_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2010.02.012_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2010.06.006_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2013.01.023_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.4294/zisin.63.139_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.4294/zisin.61.1_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2015.05.021_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2017.07.010_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.5575/geosoc.115.437_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.1029/2020jb019601_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.1002/2015jb012336_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.1186/s40623-017-0631-5_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.1186/s40645-018-0251-0_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.4294/zisin.2017-11_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.1029/2023jb027178_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.1002/2014jb011103_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.1029/2020jb021138_references_DOI_CC3rgNCIczR6iCN16iCE4iC4uIn"},{"@type":"CROSSREF","@value":"10.1029/2022jb025373_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2024.230536_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.4294/zisin.2018-1_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2014.06.009_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.1016/j.earscirev.2016.06.011_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2017.11.016_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"},{"@type":"CROSSREF","@value":"10.5917/jagh.57.415_references_DOI_2kWV5W0BBdsgJS7XUr7sjoR8lDd"}]}