{"@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/1362825895114149376.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1785/0120100263"}},{"identifier":{"@type":"URI","@value":"https://syndication.highwire.org/content/doi/10.1785/0120100263"}}],"dc:title":[{"@value":"The Optimal Use of Horizontal-to-Vertical Spectral Ratios of Earthquake Motions for Velocity Inversions Based on Diffuse-Field Theory for Plane Waves"}],"description":[{"notation":[{"@value":"The coda of earthquake motions and microtremors are sometimes referred to as diffuse-wave fields. They are generated by the multiple scattering due to the complexity of the Earth. It is accepted that the average cross correlation between the diffuse-field motions at pairs of receivers, in the frequency domain, is proportional to the imaginary part of the Green’s function between these locations. The average autocorrelation of a single receiver is also proportional to the imaginary part of the Green’s function when both the source and receiver are the same. In this study we explored the application of diffuse-field concepts to analyze earthquake records at a site when its site effect can be described using a 1D model. We derived a corollary of Claerbout’s result for a 1D layered medium. We found that the imaginary part of the Green’s function at the free surface is proportional to the square of the absolute value of the corresponding transfer function for a plane, vertically incident wave. We considered a set of incoming plane waves (of P , SV , and SH types) with varying azimuths and incidence angles. After summing up a few hundred synthetics with inclined incidences we obtained horizontal-to-vertical (H/V) spectral ratios that match the ratios estimated from the simple theory of diffuse field. By using observed records in Japan, we found that the earthquake H/V ratios are quite stable and converge rapidly regardless of what part of the waveform is used, except the P -wave part. We also found that their spectral characteristics can be reproduced well by the velocity structures estimated in previous studies. However, theory and observation were not in perfect agreement, which in turn means that the inversion of a 1D structure could be accomplished by adopting the proposed theory for earthquake H/V spectral ratios."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004236852575371","@type":"Researcher","foaf:name":[{"@value":"H. Kawase"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895114149377","@type":"Researcher","foaf:name":[{"@value":"F. J. Sanchez-Sesma"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895114149376","@type":"Researcher","foaf:name":[{"@value":"S. Matsushima"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00371106"}],"prism:publicationName":[{"@value":"Bulletin of the Seismological Society of America"}],"dc:publisher":[{"@value":"Seismological Society of America (SSA)"}],"prism:publicationDate":"2011-09-26","prism:volume":"101","prism:number":"5","prism:startingPage":"2001","prism:endingPage":"2014"},"reviewed":"false","url":[{"@id":"https://syndication.highwire.org/content/doi/10.1785/0120100263"}],"createdAt":"2011-09-26","modifiedAt":"2017-11-03","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/1050292706231200896","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Simulation of building damage distribution in downtown Mashiki, Kumamoto, Japan caused by the 2016 Kumamoto earthquake based on site-specific ground motions and nonlinear structural analyses"}]},{"@id":"https://cir.nii.ac.jp/crid/1050297372150654208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Simulation of soil liquefaction distribution in downtown Mashiki during 2016 Kumamoto earthquake using nonlinear site response"}]},{"@id":"https://cir.nii.ac.jp/crid/1050306506454177152","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Estimation of 1-D velocity models beneath strong-motion observation sites in the Kathmandu Valley using strong-motion records from moderate-sized earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1050845760771286784","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The cause of heavy damage concentration in downtown Mashiki inferred from observed data and field survey of the 2016 Kumamoto earthquake"},{"@value":"The cause of heavy damage concentration in downtown Mashiki inferred from observed data and field survey of the 2016 Kumamoto earthquake sequence and its impact on earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168779924096","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A new empirical method for obtaining horizontal site amplification factors with soil 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Records"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302865736598272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Strong-motion simulation for the 1944 Tonankai earthquake based on the statistical green’s function method and stochastic representation of complex source process"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580232384386176","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Within-site variability in earthquake site response"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588381078149632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Transfer learning model for estimating site amplification factors from limited microtremor H/V spectral ratios"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205349921920","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"STUDY ON THE CALCULATION METHOD OF EARTHQUAKE H/V SPECTRUM RATIO USING SITE AMPLIFICATION FACTOR - ON EARTHQUAKE RECORDS IN FUKUI PREFECTURE -"},{"@language":"ja","@value":"サイト増幅特性を用いた地震動H/Vスペクトルの計算法に関する考察―福井地域の地震観測記録を対象として―"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205358676352","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"地表観測記録の強震／弱震スペクトル比（S/W スペクトル）に基づく強震時における水平地震動の評価法の検討"},{"@language":"en","@value":"Examination of evaluation method of horizontal strong motions based on strong-to-weak motion (S/W) spectral ratio at the ground surface"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205358753152","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"相模トラフ沿いの中規模スラブ内地震記録に基づく表面波と散乱波を考慮した統計的グリーン関数"},{"@language":"en","@value":"Stochastic Green's Functions Considering Surface Waves and Scattering Waves Using Strong Motion Records of Moderate-Sized Intraplate Earthquakes along the Sagami Trough"},{"@value":"Stochastic Green&apos;s Functions Considering Surface Waves and Scattering Waves Using Strong Motion Records of Moderate-Sized Intraplate Earthquakes along the Sagami Trough"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205359305600","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"東北地方太平洋沖地震の際に観測された大加速度記録と周辺地盤構造の関係"},{"@language":"en","@value":"The Relation between the High-Acceleration Ground Motions Observed during the Great Tohoku Earthquake and the Surface Geology"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205359331072","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"微動と地震動観測記録及びMASW手法に基づいた港湾地域強震観測網仙台観測点におけるS波速度構造推定"},{"@language":"en","@value":"Estimation of S-wave Velocity Structures Using MASW, Microtremors, and Earthquake Motions at Port and Airport Research Institute Sendai Station"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205604787712","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"経験的グリーン関数法に基づく1855年安政江戸地震の広帯域震源モデルと首都圏及び広域での強震動の推定"},{"@language":"en","@value":"ESTIMATION OF BROADBAND SOURCE MODEL OF THE 1855 ANSEI-EDO EARTHQUAKE AND THE STRONG MOTIONS IN THE TOKYO METROPOLITAN AND REGIONAL AREA USING THE EMPIRICAL GREEN'S FUNCTION METHOD"},{"@language":"ja-Kana","@value":"ケイケンテキ グリーン カンスウホウ ニ モトズク 1855ネンアンセイ エド ジシン ノ コウタイイキ シンゲン モデル ト シュトケン オヨビ コウイキ デ ノ キョウシンドウ ノ スイテイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205605166848","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"ENVELOPE MODEL FOR STOCHASTIC GREEN'S FUNCTION METHOD USING RECORDS OF MEDIUM-SIZED EARTHQUAKES IN THE SOURCE REGION OF THE 2008 IWATE-MIYAGI NAIRIKU EARTHQUAKE"},{"@language":"ja","@value":"2008年岩手・宮城内陸地震震源域の中規模地震記録に基づく統計的グリーン関数法の経時特性モデル"},{"@language":"ja-Kana","@value":"2008ネン イワテ ・ ミヤギ ナイリク ジシン シンゲンイキ ノ チュウキボ ジシン キロク ニ モトズク トウケイテキ グリーン カンスウホウ ノ ケイジ トクセイ モデル"}]},{"@id":"https://cir.nii.ac.jp/crid/1390003825209104128","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"PARAMETER IDENTIFICATION OF LIQUEFIED SOIL MODEL FROM RECORD OF CENTRIFUGE TESTING"},{"@language":"ja","@value":"遠心載荷試験結果を用いた液状化地盤のモデルパラメータ推定"},{"@language":"ja-Kana","@value":"エンシンサイカ シケン ケッカ オ モチイタ エキジョウカ ジバン ノ モデルパラメータ スイテイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390004222629087488","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"INCORPORATING RUPTURE DIRECTIVITY EFFECTS INSIDE SUBFAULTS IN STOCHASTIC GREEN'S FUNCTION METHOD"},{"@language":"ja","@value":"要素内の破壊伝播による指向性を考慮した統計的グリーン関数法"},{"@language":"ja-Kana","@value":"ヨウソ ナイ ノ ハカイ デンパ ニ ヨル シコウセイ オ コウリョ シタ トウケイテキ グリーン カンスウホウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390007303770871936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"THE RELATIONSHIP BETWEEN HOUSING DAMAGES AND GROUND MOTION CHARACTERISTICS DUE TO THE 2016 CENTRAL TOTTORI PREFECTURE EARTHQUAKE, JAPAN"},{"@language":"ja","@value":"2016年鳥取県中部の地震における建物被害と地盤震動特性の関係"}]},{"@id":"https://cir.nii.ac.jp/crid/1390019058251828992","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Stability assessment of road rock slopes using seismic motions"}]},{"@id":"https://cir.nii.ac.jp/crid/1390024246560732544","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Inversion Analysis for Horizontal-to-Vertical Spectral Ratio of Earthquake at S-net Sites Focusing on Relatively Low Frequency Range"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680326570752","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"APPLICABILITY OF AN INVERSION OF EARTHQUAKE H/V SPECTRAL RATIOS FOR SOIL STRUCTURES - A CASE STUDY USING RECORDS IN FUKUI PREFECTURE"},{"@language":"ja","@value":"地震動H/Vスペクトルによる地盤構造逆解析の適用性―福井地域の記録を用いた事例研究ー"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680334467712","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"微動と地震動の観測水平上下スペクトル比の相違とそれに着目した地盤構造同定手法の提案"},{"@language":"en","@value":"Comparison of Observed Earthquake and Microtremor Horizontal-to-Vertical Spectral Ratios and Inversion of Velocity Structures Based on Their Empirical Ratios"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680335464960","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"スペクトルインバージョン手法に基づく強震動特性の統計的性質に関する研究"},{"@language":"en","@value":"Statistical properties of strong ground motions based on the spectral inversion method,"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680582476928","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"改良統計的グリーン関数法に基づく1923年関東地震の強震動生成域と強震動の推定"},{"@language":"en","@value":"ESTIMATION OF STRONG MOTION GENERATION AREAS AND STRONG MOTIONS DURING THE 1923 KANTO EARTHQUAKE USING REVISED STOCHASTIC GREEN'S FUNCTION METHOD"},{"@language":"ja-Kana","@value":"カイリョウ トウケイテキ グリーン カンスウホウ ニ モトズク 1923ネン カントウ ジシン ノ キョウシンドウ セイセイイキ ト キョウシンドウ ノ スイテイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680582508288","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"GENERATION METHOD OF STOCHASTIC GREEN'S FUNCTION CONSIDERING INTO SURFACE WAVES AND SCATTERING WAVES USING RECORDS OF MODERATE-SIZED INTERPLATE EARTHQUAKES ALONG THE SAGAMI TROUGH"},{"@language":"ja","@value":"相模トラフ沿いの中規模地震の観測記録に基づく表面波と散乱波を考慮した統計的グリーン関数生成方法"},{"@language":"ja-Kana","@value":"サガミ トラフ ゾイ ノ チュウキボ ジシン ノ カンソク キロク ニ モトズク ヒョウメンハ ト サンランハ オ コウリョ シタ トウケイテキ グリーン カンスウ セイセイ ホウホウ"},{"@value":"GENERATION METHOD OF STOCHASTIC GREEN^|^apos;S FUNCTION CONSIDERING INTO SURFACE WAVES AND SCATTERING WAVES USING RECORDS OF MODERATE-SIZED INTERPLATE EARTHQUAKES ALONG THE SAGAMI TROUGH"},{"@value":"Generation method of stochastic Green’s function considering into surface waves and scattering waves using records of moderate‐size interplate earthquakes along the Sagami trough"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681463204480","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Relationship between Building Damage Ratios and Ground Motion Characteristics during the 2011 Tohoku Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282763129714048","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The relationship between Vs, Vp and depth based on PS-logging data at K-NET and KiK-net sites"},{"@language":"ja","@value":"K-NET・KiK-netのPS検層記録に基づくVs・Vpおよび深さの関係"},{"@language":"ja-Kana","@value":"K-NET ・ KiK-net ノ PSケンソウ キロク ニ モトズク Vs ・ Vp オヨビ フカサ ノ カンケイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390300533228710528","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Site response at the Dobutsu station in Aomori prefecture, Japan during strong and weak earthquake ground motion"}]},{"@id":"https://cir.nii.ac.jp/crid/1390580295553264640","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Seismic observations of a deep-seated landslide site in Sambagawa Belt"},{"@language":"ja","@value":"三波川帯における深層崩壊斜面の地震動計測"}]},{"@id":"https://cir.nii.ac.jp/crid/1390582008205403904","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Evaluation of site amplification factors at severely damaged sites during the 1923 Kanto Earthquake by using 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