{"@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/1390282679280144768.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.4294/zisin1948.36.3_351"}},{"identifier":{"@type":"DOI","@value":"10.4294/zisin1948.25.1_44"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"7551070"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/7551070"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I7551070"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"2969223"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/2969223"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I2969223"}},{"identifier":{"@type":"URI","@value":"https://www.jstage.jst.go.jp/article/zisin1948/36/3/36_3_351/_pdf"}},{"identifier":{"@type":"URI","@value":"https://www.jstage.jst.go.jp/article/zisin1948/25/1/25_1_44/_pdf"}},{"identifier":{"@type":"NAID","@value":"130006785783"}},{"identifier":{"@type":"NAID","@value":"10006221108"}},{"identifier":{"@type":"NAID","@value":"130006784045"}},{"identifier":{"@type":"NAID","@value":"40017853368"}}],"dc:title":[{"@language":"ja","@value":"三河地震における深溝断層の屈曲部について"},{"@language":"en","@value":"The Turning of the Fukozu Fault Associated with the Mikawa Earthquake in 1945"},{"@value":"三河地震における深溝断層の延長部について"},{"@language":"ja-Kana","@value":"ミカワ ジシン ニ オケル フカミゾ ダンソウ ノ エンチョウブ ニ ツイテ"},{"@language":"ja-Kana","@value":"ミカワ ジシン ニ オケル フコウズ ダンソウ ノ クッキョクブ ニ ツイテ"},{"@value":"The Extension of the Fukozu Fault Associated with the Mikawa Earthquake in 1945"}],"description":[{"type":"abstract","notation":[{"@language":"en","@value":"The turning of the Fukozu fault associated with the 1945 Mikawa earthquake was investigated by the present geological survey. It was ascertained that the fault had two continuous bends designated the first and third bend, and two discontinuous bends designated the second and fourth bend. Consequently the Fukozu fault is considered to be composed of three separated earthquake faults.<br>Judging from the formation of these faults, their major features may be explained as the results of an east-northeastward upthrusting of three land blocks on the west-southwestern sides of the faults.<br>These three faults are all active ones and the left-lateral displacement along the WSWENE course of the first fault (from Atsumi Bay to Maeno) has presumably accumulated in the same direction, a total distance being about 450m. Our survey, moreover, revealed that the west-southwestern extension of the WSW-ENE course of the first fault might be probably an active fault."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1410282679280144769","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000391401398"},{"@type":"NRID","@value":"9000391402936"}],"foaf:name":[{"@language":"ja","@value":"坂部 和夫"},{"@language":"en","@value":"SAKABE Kazuo"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Hekinan Senior High School, Aichi Prefecture"},{"@language":"ja","@value":"愛知県立碧南高等学校"}]},{"@id":"https://cir.nii.ac.jp/crid/1410282679280144768","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000391401399"},{"@type":"NRID","@value":"9000391402935"},{"@type":"NRID","@value":"9000002265716"}],"foaf:name":[{"@language":"ja","@value":"飯田 汲事"},{"@language":"en","@value":"IIDA Kumiji"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Aichi Institute of Technology"},{"@language":"ja","@value":"愛知工業大学"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00371114"},{"@type":"LISSN","@value":"00371114"},{"@type":"EISSN","@value":"18839029"},{"@type":"EISSN","@value":"2186599X"},{"@type":"NDL_BIB_ID","@value":"000000009860"},{"@type":"ISSN","@value":"00371114"},{"@type":"PISSN","@value":"http://id.crossref.org/issn/00371114"},{"@type":"NCID","@value":"AN00305741"}],"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":"1983","prism:volume":"36","prism:number":"3","prism:startingPage":"351","prism:endingPage":"358"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"http://id.ndl.go.jp/bib/7551070"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I7551070"},{"@id":"http://id.ndl.go.jp/bib/2969223"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I2969223"},{"@id":"https://www.jstage.jst.go.jp/article/zisin1948/36/3/36_3_351/_pdf"},{"@id":"https://www.jstage.jst.go.jp/article/zisin1948/25/1/25_1_44/_pdf"}],"availableAt":"1983","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1390001204303386368","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Re-examination of Ground Deformation and Fault Models of the 1945 Mikawa Earthquake (<I>M</I> =6.8)"},{"@value":"1945年三河地震（<I>M</I> ＝6.8）に伴う地殻変動と震源断層モデルの再検討"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204306602496","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"深溝断層におけるガンマ線の強度"},{"@language":"en","@value":"Gamma Ray Intensity Surrounding the Fukouzu Fault"},{"@language":"ja-Kana","@value":"フコウズ ダンソウ ニ オケル ガンマセン ノ キョウド"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205600843776","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"CHARACTERISTICS OF SURFACE FAULT RUPTURE RELATING TO MAGNITUDE AND SLIP TYPE OF INLAND EARTHQUAKES"},{"@language":"ja","@value":"内陸地震の規模・タイプと地表地震断層の特性との関係"},{"@language":"ja-Kana","@value":"ナイリク ジシン ノ キボ タイプ ト チヒョウ ジシン ダンソウ ノ トクセイ ト ノ カンケイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206513406976","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Source rupture processes of the 1944 Tonankai earthquake and the 1945 Mikawa earthquake 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