{"@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/1390282681505043584.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.11456/shigenchishitsu1951.36.209"}},{"identifier":{"@type":"NAID","@value":"130003639697"}}],"dc:title":[{"@language":"en","@value":"Neogene regional stress field inferred from the pattern of ore veins in Hokkaido, Japan"},{"@value":"鉱脈の方向から推定された広域応力場"}],"dcterms:alternative":[{"@value":"北海道における中期中新世以降の鉱脈の例"}],"description":[{"type":"abstract","notation":[{"@language":"en","@value":"Neogene stress field in Hokkaido has been analyzed, based on the strikes of ore veins. The ore veins formed during the period from late Middle Miocene to Recent are taken into account. Those of E-W and ENE-WSW directions are predominant in both northeast and southwest Hokkaido.<BR>The major veins of thirteen representative mines are formed in the conjugate shear fractures, that is, E-W or ENE-WSW dextral and NW-SE sinistral. The estimated stress field is NW-SE or WNW-ESE compressional and parallel to the direction of the subducting Pacific Plate, even at ore-forming period. The predominance of E-W and ENE-WSW dextral shears might be related to the oblique subduction of the Pacific Plate."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1410290696752936450","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000253483651"}],"foaf:name":[{"@language":"en","@value":"WATANABE Yasushi"},{"@language":"ja","@value":"渡辺 寧"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Hokkaido Branch, Geological survey of Japan,"},{"@language":"ja","@value":"地質調査所北海道支所"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00265209"}],"prism:publicationName":[{"@language":"en","@value":"Mining Geology"},{"@language":"ja","@value":"鉱山地質"},{"@language":"en","@value":"Mining Geology"},{"@language":"en","@value":"Kozan chishitsu"},{"@language":"ja","@value":"鉱山地質"}],"dc:publisher":[{"@language":"en","@value":"The Society of Resource Geology"},{"@language":"ja","@value":"資源地質学会"}],"prism:publicationDate":"1986","prism:volume":"36","prism:number":"197","prism:startingPage":"209","prism:endingPage":"218"},"availableAt":"1986","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Ore%20vein","dc:title":"Ore vein"},{"@id":"https://cir.nii.ac.jp/all?q=Stress%20field","dc:title":"Stress field"},{"@id":"https://cir.nii.ac.jp/all?q=Shear%20fracture","dc:title":"Shear fracture"},{"@id":"https://cir.nii.ac.jp/all?q=Tension%20fracture","dc:title":"Tension fracture"},{"@id":"https://cir.nii.ac.jp/all?q=%C3%89chelon","dc:title":"Échelon"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1390282763082938240","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Ore–microscopy and Geochemistry of Gold–Silver Telluride Mineralization in Southwestern Hokkaido, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842051746432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatiotemporal variations in the stress field in the northeasternmost part of the NE Japan arc : constraints from microearthquakes"}]}],"dataSourceIdentifier":[{"@type":"JALC","@value":"oai:japanlinkcenter.org:0038960361"},{"@type":"CIA","@value":"130003639697"},{"@type":"CROSSREF","@value":"10.1186/s40623-020-01245-8_references_DOI_8lHA9TWeFttAJ0MSusxM6S9UQNY"},{"@type":"CROSSREF","@value":"10.2465/jmps.171017_references_DOI_8lHA9TWeFttAJ0MSusxM6S9UQNY"}]}