{"@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/1881428067690792832.json","@type":"Dataset","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.6084/m9.figshare.17138672.v4"}},{"identifier":{"@type":"DOI","@value":"10.6084/m9.figshare.17138672"}},{"identifier":{"@type":"DOI","@value":"10.6084/m9.figshare.17138672.v3"}}],"dc:title":[{"@value":"3DS_WAVE_VELOCITYMODEL_EPS.dat"}],"description":[{"notation":[{"@value":"The first column in the provided text file for the S-wave velocity model represents the Latitude, second column is the Longitude, third column is the depth (after topography correction), the fourth column is the S-wave velocity.<br>We also provide the input text file for the parameters used in the inversion."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1891428067690792832","@type":"Researcher","foaf:name":[{"@value":"NTHABA, BOKANI"}]}],"publication":{"dc:publisher":[{"@value":"figshare"}],"prism:publicationDate":"2022-01-01"},"dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/2051714792015349120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Ambient noise tomography for a high-resolution 3D S-wave velocity model of the Kinki Region, Southwestern Japan, using dense seismic array data"}]}],"dataSourceIdentifier":[{"@type":"OPENAIRE","@value":"doi_dedup___::38bb9cf0a6e2b4f50b7ec087a536ea45"}]}