{"@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/1390282679526123136.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.2343/geochemj.19.237"}},{"identifier":{"@type":"COI","@value":"1:CAS:528:DyaL28XosFWi"}},{"identifier":{"@type":"URI","@value":"http://www.jstage.jst.go.jp/article/geochemj1966/19/4/19_4_237/_pdf"}},{"identifier":{"@type":"NAID","@value":"130003904351"}}],"dc:title":[{"@language":"en","@value":"High initial Sr-isotopic ratios of gabbro and metadiabase in the Ryoke Belt, Southwest Japan."}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"Rb and Sr contents and Sr-isotopic ratios as well as SiO<sub>2</sub> and K<sub>2</sub>O contents were determined for basic rocks (gabbro, cortlandite, anorthosite and metadiabase) from the Ryoke Belt in the Kinki and Setouchi Inland Sea districts, Southwest Japan. The basic rocks are characterized by lower K<sub>2</sub>O and Rb contents and by higher initial Sr-isotopic ratios than the mantle-derived igneous rocks in the oceanic region. The high initial Sr-isotopic ratios of the basic rocks are explained by the high isotopic ratios of their source materials."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1410282679526123139","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000254578616"}],"foaf:name":[{"@language":"en","@value":"Kagami Hiroo"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Institute for Thermal Spring Research, Okayama University"}]},{"@id":"https://cir.nii.ac.jp/crid/1410282679526123137","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000254578617"}],"foaf:name":[{"@language":"en","@value":"Tainosho Yoshiaki"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Department of Geology, Faculty of Education, Kobe University"}]},{"@id":"https://cir.nii.ac.jp/crid/1030003658319480583","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"80032639"},{"@type":"NRID","@value":"1000080032639"},{"@type":"NRID","@value":"9000002661516"},{"@type":"NRID","@value":"9000003184448"},{"@type":"NRID","@value":"9000006082385"},{"@type":"NRID","@value":"9000006081063"},{"@type":"NRID","@value":"9000006910691"},{"@type":"NRID","@value":"9000006082380"},{"@type":"NRID","@value":"9000270170138"},{"@type":"NRID","@value":"9000270170144"},{"@type":"NRID","@value":"9000006081077"},{"@type":"NRID","@value":"9000006081079"},{"@type":"NRID","@value":"9000270169850"},{"@type":"NRID","@value":"9000003183880"},{"@type":"NRID","@value":"9000006081075"},{"@type":"NRID","@value":"9000006081042"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0015814"}],"foaf:name":[{"@language":"en","@value":"Iizumi Shigeru"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Institute of Geology, Faculty of Science, Shimane University"}]},{"@id":"https://cir.nii.ac.jp/crid/1410282679526123138","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000254578619"}],"foaf:name":[{"@language":"en","@value":"Hayama Yoshikazu"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Geological Institute, Tokyo University of Agriculture"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00167002"},{"@type":"LISSN","@value":"00167002"},{"@type":"EISSN","@value":"18805973"},{"@type":"PISSN","@value":"http://id.crossref.org/issn/00167002"}],"prism:publicationName":[{"@language":"en","@value":"GEOCHEMICAL JOURNAL"},{"@language":"ja","@value":"ＧＥＯＣＨＥＭＩＣＡＬ　ＪＯＵＲＮＡＬ"},{"@language":"en","@value":"Geochem. J."},{"@language":"ja","@value":"Ｇｅｏｃｈｅｍ．　Ｊ．"}],"dc:publisher":[{"@language":"en","@value":"GEOCHEMICAL SOCIETY OF JAPAN"},{"@language":"ja","@value":"一般社団法人日本地球化学会"}],"prism:publicationDate":"1985","prism:volume":"19","prism:number":"4","prism:startingPage":"237","prism:endingPage":"243"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"http://www.jstage.jst.go.jp/article/geochemj1966/19/4/19_4_237/_pdf"}],"availableAt":"1985","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Geochemistry%20and%20Petrology","dc:title":"Geochemistry and Petrology"},{"@id":"https://cir.nii.ac.jp/all?q=Geophysics","dc:title":"Geophysics"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360848656205401984","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geochemical characteristics of hydrous basaltic magmas due to assimilation and fractional crystallization: the Ikoma gabbroic complex, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679205666048","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Cretaceous Events at the Eastern Margin of East Asia Recorded in Rocks of the Ryoke Belt, SW Japan"},{"@language":"ja","@value":"領家帯に記録された東アジア東縁の白亜紀イベント"},{"@language":"ja-Kana","@value":"リョウケタイ ニ キロク サレタ ヒガシアジア トウエン ノ ハクアキ イベント"},{"@value":"Cretaceous events at the eastern margin of the East Asia recorded in rocks of the Ryoke belt,"}]},{"@id":"https://cir.nii.ac.jp/crid/1390297216596711936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Zircon U-Pb ages of the Cretaceous gabbroic and granitic rocks from the Kajishima, northwest Shikoku, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390575751443798016","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Origin of xenoliths within the Hime–shima volcanic group, Kyushu, southwestern Japan Arc"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942186658176","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geochemical and mineralogical characteristics of fault gouge in the Median Tectonic Line, Japan : evidence for earthquake slip"}]}],"dataSourceIdentifier":[{"@type":"JALC","@value":"oai:japanlinkcenter.org:0020708314"},{"@type":"CROSSREF","@value":"10.2343/geochemj.19.237"},{"@type":"CIA","@value":"130003904351"},{"@type":"OPENAIRE","@value":"doi_dedup___::e2560f516f68297fff8c2c64551a30d3"},{"@type":"CROSSREF","@value":"10.1186/1880-5981-66-36_references_DOI_98Pw95Oreorz1RWydo7xr2hNtp4"},{"@type":"CROSSREF","@value":"10.5026/jgeography.120.452_references_DOI_98Pw95Oreorz1RWydo7xr2hNtp4"},{"@type":"CROSSREF","@value":"10.2465/jmps.211217b_references_DOI_98Pw95Oreorz1RWydo7xr2hNtp4"},{"@type":"CROSSREF","@value":"10.2465/jmps.230224_references_DOI_98Pw95Oreorz1RWydo7xr2hNtp4"},{"@type":"CROSSREF","@value":"10.1007/s00710-016-0423-9_references_DOI_98Pw95Oreorz1RWydo7xr2hNtp4"}]}