{"@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/1361699994790156032.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.geomorph.2008.02.012"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0169555X08000603?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0169555X08000603?httpAccept=text/plain"}}],"dc:title":[{"@value":"A fault scarp in an urban area identified by LiDAR survey: A Case study on the Itoigawa–Shizuoka Tectonic Line, central Japan"}],"description":[{"notation":[{"@value":"Abstract   A light detection and ranging (LiDAR) survey was conducted in a densely built-up area to generate a high-resolution digital elevation model (DEM) to look for active faults. The urban district of Matsumoto City in central Japan is located in a 3-km 2  basin along the Itoigawa–Shizuoka Tectonic Line active fault system, one of Japanese onshore fault systems with the highest earthquake probability. A high-resolution DEM at a 0.5-m-grid interval was obtained after removing the effects of laser returns from buildings, clouds and vegetation. It revealed a continuous scarp, up to ~ 2 m in height. Borehole data and archaeological studies indicate the scarp was formed during the most recent faulting event associated with historical earthquakes. In addition, the fault scarp strongly supports that the urban district is in a pull-apart basin related to a fault step-over between two left-lateral strike-slip faults. Consequently, accurate interpretation of fault geometry is crucial to provide estimates of future surface deformation and to allow modeling of basin structure and strong ground motion. Thus, the LiDAR mapping survey in urban districts is effective for detailed active fault mapping in order to constrain basin structure and to forecast the exact location of surface rupturing associated with large earthquakes."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380567007856030346","@type":"Researcher","foaf:name":[{"@value":"H. Kondo"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699994790156161","@type":"Researcher","foaf:name":[{"@value":"S. Toda"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699994790156033","@type":"Researcher","foaf:name":[{"@value":"K. Okumura"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699994790156034","@type":"Researcher","foaf:name":[{"@value":"K. Takada"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699994790156032","@type":"Researcher","foaf:name":[{"@value":"T. Chiba"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"0169555X"}],"prism:publicationName":[{"@value":"Geomorphology"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2008-11","prism:volume":"101","prism:number":"4","prism:startingPage":"731","prism:endingPage":"739"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0169555X08000603?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0169555X08000603?httpAccept=text/plain"}],"createdAt":"2008-03-12","modifiedAt":"2019-05-08","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360285707500092672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Investigating the role of the Itoigawa-Shizuoka tectonic line towards the evolution of the Northern Fossa Magna rift basin"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182122906368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Detection of subtle tectonic–geomorphic features in densely forested mountains by very high-resolution airborne LiDAR survey"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182476880000","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismological evidence of an active footwall shortcut thrust in the Northern Itoigawa–Shizuoka Tectonic Line derived by the aftershock sequence of the 2014 M 6.7 Northern Nagano earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206239553152","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Surface rupture and slip associated with the 2014 Nagano-ken Hokubu earthquake（Mw6.2）"},{"@language":"ja","@value":"2014年長野県北部の地震（Mw6.2）に伴う地表地震断層の分布と変位量"},{"@language":"ja-Kana","@value":"2014ネン ナガノケン ホクブ ノ ジシン(Mw6.2)ニ トモナウ チヒョウ ジシン ダンソウ ノ ブンプ ト ヘンイリョウ"},{"@value":"Surface rupture and slip associated with the 2014 Nagano‐ken Hokubu earthquake (Mw 6.2)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282763076663808","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Progress of active fault studies in Japan in the past 25 years and future prospects"},{"@language":"ja","@value":"我が国における活断層研究の最近25年の成果と今後の展望"},{"@language":"ja-Kana","@value":"ワガクニ ニ オケル カツダンソウ ケンキュウ ノ サイキン 25ネン ノ セイカ ト コンゴ ノ テンボウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390300302109572864","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Long-term forecast and occurrence probability based on past multi-segment megaquakes on the ISTL active fault zone"},{"@language":"ja","@value":"糸魚川-静岡構造線断層帯における連動型巨大地震の発生可能性評価"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942122898304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dynamic rupture propagation on geometrically complex fault with along-strike variation of fault maturity : insights from the 2014 Northern Nagano earthquake"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/j.geomorph.2008.02.012"},{"@type":"OPENAIRE","@value":"doi_dedup___::2b4ad990eb4b6291bbf410ae1a91b950"},{"@type":"CROSSREF","@value":"10.1186/s40623-017-0715-2_references_DOI_2qRUKw8Lp0Q9CVM5BFRvCqy0omZ"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2018.0028_references_DOI_2qRUKw8Lp0Q9CVM5BFRvCqy0omZ"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2016.04.019_references_DOI_2qRUKw8Lp0Q9CVM5BFRvCqy0omZ"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2013.12.014_references_DOI_2qRUKw8Lp0Q9CVM5BFRvCqy0omZ"},{"@type":"CROSSREF","@value":"10.4116/jaqua.63.2219_references_DOI_2qRUKw8Lp0Q9CVM5BFRvCqy0omZ"},{"@type":"CROSSREF","@value":"10.1016/j.geomorph.2012.11.001_references_DOI_2qRUKw8Lp0Q9CVM5BFRvCqy0omZ"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2016.0048_references_DOI_2qRUKw8Lp0Q9CVM5BFRvCqy0omZ"}]}