{"@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/1361981469894920064.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.1078551"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.1078551"}}],"dc:title":[{"@value":"Long-Range Correlations in the Diffuse Seismic Coda"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The late seismic coda may contain coherent information about the elastic response of Earth. We computed the correlations of the seismic codas of 101 distant earthquakes recorded at stations that were tens of kilometers apart. By stacking cross-correlation functions of codas, we found a low-frequency coherent part in the diffuse field. The extracted pulses have the polarization characteristics and group velocities expected for Rayleigh and Love waves. The set of cross-correlations has the symmetries of the surface-wave part of the Green tensor. This seismological example shows that diffuse waves produced by distant sources are sufficient to retrieve direct waves between two perfectly located points of observation. Because it relies on general properties of diffuse waves, this result has potential applications in other fields.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381981469894920064","@type":"Researcher","foaf:name":[{"@value":"Michel Campillo"}],"jpcoar:affiliationName":[{"@value":"Laboratoire de Géophysique Interne et Tectonophysique, Observatoire de Grenoble, Université Joseph Fourier & CNRS, BP 53, 38041 Grenoble, France."}]},{"@id":"https://cir.nii.ac.jp/crid/1381981469894920065","@type":"Researcher","foaf:name":[{"@value":"Anne Paul"}],"jpcoar:affiliationName":[{"@value":"Laboratoire de Géophysique Interne et Tectonophysique, Observatoire de Grenoble, Université Joseph Fourier & CNRS, BP 53, 38041 Grenoble, France."}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00368075"},{"@type":"EISSN","@value":"10959203"}],"prism:publicationName":[{"@value":"Science"}],"dc:publisher":[{"@value":"American Association for the Advancement of Science (AAAS)"}],"prism:publicationDate":"2003-01-24","prism:volume":"299","prism:number":"5606","prism:startingPage":"547","prism:endingPage":"549"},"reviewed":"false","url":[{"@id":"https://www.science.org/doi/pdf/10.1126/science.1078551"}],"createdAt":"2003-01-23","modifiedAt":"2024-12-11","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001338209108864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Difference of horizontal-to-vertical spectral ratios of observed earthquakes and microtremors and its application to S-wave velocity inversion based on the diffuse field concept"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216708238976","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Temporal change of phase velocity beneath Mt. 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Scalar Waves"},{"@language":"ja","@value":"波動場の空間相関とグリーン関数との関係のスローネス法に基づく導出: 等方入射するランダムスカラー波の場合"},{"@language":"ja-Kana","@value":"ハドウバ ノ クウカン ソウカン ト グリーン カンスウ トノ カンケイ ノ スローネスホウ ニ モトズク ドウシュツ トウホウ ニュウシャスル ランダム スカラーハ ノ バアイ"},{"@value":"A Derivation of the Relation between Spatial Correlation and Green^|^rsquo;s Function Based on the Slowness Method: Isotropic Incidence of Random Scalar Waves"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206495136512","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"地震波干渉法を用いた近地自然地震Pコーダ波による地殻構造探査"},{"@language":"en","@value":"Subsurface exploration with P-coda of local earthquakes using seismic interferometry"},{"@language":"ja-Kana","@value":"ジシンハ カンショウホウ オ モチイタ キン チ シゼン ジシン Pコーダハ ニ ヨル チカク コウゾウ タンサ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206496130176","@type":"Article","resourceType":"学術雑誌論文(journal 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interferometry"},{"@language":"ja","@value":"地震波干渉法による地下構造イメージング技術の実用化にむけた実験的研究"}]},{"@id":"https://cir.nii.ac.jp/crid/1390845713075817472","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Applicability of phase velocity estimation method using Green's functions with a common virtual source from seismic interferometry - In the case of the Wakasa bay region considering asymmetry of cross-correlation functions of ambient noise -"},{"@language":"ja","@value":"地震波干渉法による共通仮想震源によるグリーン関数を用いた位相速度推定法の適用性―常時微動の相互相関関数の非対称性に着目した若狭湾地域における検討―"},{"@language":"ja-Kana","@value":"ジシンハ カンショウホウ ニ ヨル キョウツウ カソウ シンゲン ニ ヨル グリーン カンスウ オ モチイタ イソウ ソクド スイテイホウ ノ テキヨウセイ : ジョウジ ビドウ ノ ソウゴ ソウカン カンスウ ノ ヒタイショウセイ ニ チャクモク シタ ワカサワン チイキ ニ オケル ケントウ"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367120486400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geographical distribution of shear wave 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