{"@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/1390282679280493312.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.4294/zisin.64.91"}},{"identifier":{"@type":"NAID","@value":"130004562080"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@language":"en","@value":"Inversion Analyses Based on ABIC with Non-full Rank Prior Information"},{"@language":"ja","@value":"ＡＢＩＣを用いたインバージョン解析：先験的拘束条件がフルランクでない場合の取り扱い"}],"dc:language":"ja","description":[{"type":"abstract","notation":[{"@language":"en","@value":"In inversion analyses using ABIC, a non-full rank matrix for prior constraints is allowed in the formulation of Yabuki and Matsu'ura (1992), while Fukuda and Johnson (2008) claimed that the matrix must be full rank. This problem depends on consideration about the value of “zero” of zero eigenvalues contained in the prior constraint matrix. In actual inversion analyses, we must have some prior information about model parameters, even if it is not explicitly expressed. Therefore, the “zero” of the zero eigenvalues is considered to be not zero exactly. Based on this consideration, we can obtain the same inversion solution as Yabuki and Matsu'ura (1992). Mathematical difficulty in expressing the prior probability density function for a matrix with zero eigenvalues can be avoided by the use of non-informative prior."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420001326217002624","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"10313206"},{"@type":"NRID","@value":"1000010313206"},{"@type":"ORCID","@value":"0000-0002-1009-7366"},{"@type":"NRID","@value":"9000413917373"},{"@type":"NRID","@value":"9000398821083"},{"@type":"NRID","@value":"9000000119384"},{"@type":"NRID","@value":"9000014597641"},{"@type":"NRID","@value":"9000402114784"},{"@type":"NRID","@value":"9000238106305"},{"@type":"NRID","@value":"9000291598334"},{"@type":"NRID","@value":"9000402114717"},{"@type":"NRID","@value":"9000405103759"},{"@type":"NRID","@value":"9000406034849"},{"@type":"NRID","@value":"9000024313830"},{"@type":"NRID","@value":"9000391405640"},{"@type":"NRID","@value":"9000405103753"},{"@type":"NRID","@value":"9000256898314"},{"@type":"NRID","@value":"9000256898260"},{"@type":"NRID","@value":"9000382634092"},{"@type":"NRID","@value":"9000410320299"},{"@type":"NRID","@value":"9000405103741"},{"@type":"NRID","@value":"9000399261878"},{"@type":"NRID","@value":"9000413695936"},{"@type":"NRID","@value":"9000410320337"},{"@type":"NRID","@value":"9000258413579"},{"@type":"NRID","@value":"9000413498697"},{"@type":"NRID","@value":"9000413497528"},{"@type":"NRID","@value":"9000297476953"},{"@type":"NRID","@value":"9000258415640"},{"@type":"NRID","@value":"9000256898266"},{"@type":"NRID","@value":"9000023929633"},{"@type":"NRID","@value":"9000023647213"},{"@type":"NRID","@value":"9000242243632"},{"@type":"NRID","@value":"9000344128696"},{"@type":"NRID","@value":"9000251870054"},{"@type":"NRID","@value":"9000402114715"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/Y_Fukahata"}],"foaf:name":[{"@language":"en","@value":"FUKAHATA Yukitoshi"},{"@language":"ja","@value":"深畑 幸俊"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Research Center for Earthquake Prediction, Disaster Prevention Research Institute, Kyoto University"},{"@language":"ja","@value":"京都大学防災研究所地震予知研究センター"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00371114"},{"@type":"LISSN","@value":"00371114"},{"@type":"EISSN","@value":"18839029"},{"@type":"EISSN","@value":"2186599X"}],"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":"2012","prism:volume":"64","prism:number":"2","prism:startingPage":"91","prism:endingPage":"95"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","availableAt":"2012","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=ABIC","dc:title":"ABIC"},{"@id":"https://cir.nii.ac.jp/all?q=Prior%20constraint","dc:title":"Prior constraint"},{"@id":"https://cir.nii.ac.jp/all?q=Zero%20eigenvalue","dc:title":"Zero eigenvalue"},{"@id":"https://cir.nii.ac.jp/all?q=Non-informative%20prior","dc:title":"Non-informative prior"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040282257057114496","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"21540428"},{"@type":"JGN","@value":"JP21540428"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-21540428/"}],"notation":[{"@language":"ja","@value":"モデリング誤差に起因する共分散成分を考慮した震源過程解析手法の確立"},{"@language":"en","@value":"Seismic source inversion with data covariance components due to modeling errors"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050564285755914880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Source Rupture Process of the Tecomán, Colima, Mexico Earthquake of 22 January 2003, Determined by Joint Inversion of Teleseismic Body-Wave and Near-Source Data"},{"@value":"Source Rupture Process of the Tecoman, Colima, Mexico Earthquake of 22 January 2003, Determined by Joint Inversion of Teleseismic Body-Wave and 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