{"@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/1363670318406567936.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2007jb005395"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2007JB005395"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2007JB005395"}}],"dc:title":[{"@value":"Three‐dimensional crustal <i>S</i> wave velocity structure in Japan using microseismic data recorded by Hi‐net tiltmeters"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>We developed a three‐step method for three‐dimensional (3‐D) <jats:italic>S</jats:italic> wave velocity tomography by fitting synthetic cross spectra to the observed ones of ambient seismic noise. We applied this method to the recording of Hi‐net tiltmeters in Japan at 679 stations from June 2004 to December 2004. First, we calculated normalized cross spectra between radial components and those between transverse components for every pair of stations. The first step is local 1‐D <jats:italic>S</jats:italic> wave velocity inversion for each station assuming small lateral heterogeneity under a 100‐km circle of a station. We measured the dispersion curves of fundamental Rayleigh waves, fundamental Love waves, and first overtone of Love waves by fitting the synthetic cross spectra to the observed ones between pairs of stations within the circle. We inverted the measured dispersion curves for obtaining a 1‐D <jats:italic>S</jats:italic> wave velocity model. The second step is the inversion of the observed cross spectra for obtaining path‐averaged 1‐D <jats:italic>S</jats:italic> wave velocity structure. The third step is the inversion of the resultant path‐averaged structures for obtaining 3‐D <jats:italic>S</jats:italic> wave velocity structure (0.1° × 0.1° × 1 km grid from the surface to a depth of 50 km) using ray approximation. The resultant <jats:italic>S</jats:italic> wave velocity structures show clear low‐velocity anomalies along tectonic lines from the surface to a depth of 20 km. In particular, along the Hidaka mountain range, we observed <jats:italic>S</jats:italic> wave perturbation more extreme than −20%. They also show low‐velocity anomalies under volcanoes in Kyusyu and Tohoku. In the southwestern part of Shikoku, our results show a clear low‐velocity anomaly corresponding to an accretional belt (Shimanto belt). Below 20 km, we observe a low‐velocity anomaly in the center of Japan, which suggests a thick crust.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380008211929843598","@type":"Researcher","foaf:name":[{"@value":"K. Nishida"}],"jpcoar:affiliationName":[{"@value":"Earthquake Research Institute University of Tokyo  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318406567938","@type":"Researcher","foaf:name":[{"@value":"H. Kawakatsu"}],"jpcoar:affiliationName":[{"@value":"Earthquake Research Institute University of Tokyo  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318406567937","@type":"Researcher","foaf:name":[{"@value":"K. Obara"}],"jpcoar:affiliationName":[{"@value":"National Research Institute for Earth Science and Disaster Prevention  Tsukuba Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2008-10","prism:volume":"113","prism:number":"B10","prism:startingPage":"B10302"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2007JB005395"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2007JB005395"}],"createdAt":"2008-10-01","modifiedAt":"2023-10-13","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050025031479234816","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Estimation of azimuthal anisotropy in the NW Pacific from seismic ambient noise in seafloor records"}]},{"@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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Hi-net レンゾク ジシン カンソク キロク オ モチイタ ジシンハ カンショウホウ ニ モトズク ケンショウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206496439296","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"地殻・上部マントルでの減衰<br/>─トモグラフィ手法によるQ値評価とその利用─"},{"@language":"en","@value":"Attenuation structure at crust and upper mantle<br/>—Estimation of Q<sub>s</sub>-value by tomographic analysis and its applications—"},{"@value":"地殻・上部マントルでの減衰 : トモグラフィ手法によるQ値評価とその利用"},{"@language":"ja-Kana","@value":"チカク ・ ジョウブ マントル デ ノ ゲンスイ : トモグラフィ シュホウ ニ ヨル Qチ ヒョウカ ト ソノ リヨウ"},{"@value":"Attenuation structure at crust and upper mantle<br/>&mdash;Estimation of Q<sub>s</sub>-value by tomographic analysis and its applications&mdash;"}]},{"@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/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/1390856660872292224","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Recent volcanic activity at the Asama volcano and long-period seismic signals"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942155084672","@type":"Article","resourceType":"学術雑誌論文(journal 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