{"@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/1362825894922384512.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/s0040-1951(00)00106-2"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0040195100001062?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0040195100001062?httpAccept=text/plain"}}],"dc:title":[{"@value":"Geologic framework and tectonic evolution of the Qinling orogen, central China"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382825894922384512","@type":"Researcher","foaf:name":[{"@value":"Qing-Ren Meng"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825894922384513","@type":"Researcher","foaf:name":[{"@value":"Guo-Wei Zhang"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00401951"}],"prism:publicationName":[{"@value":"Tectonophysics"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2000-08","prism:volume":"323","prism:number":"3-4","prism:startingPage":"183","prism:endingPage":"196"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0040195100001062?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0040195100001062?httpAccept=text/plain"}],"createdAt":"2002-10-15","modifiedAt":"2020-01-08","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001335797000192","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tectonic activity and structural features of active intracontinental normal faults in the Weihe Graben, central China"},{"@value":"Tectonic activity and structural features of intracontinental active normal faults in the Weihe Graben, central China"}]},{"@id":"https://cir.nii.ac.jp/crid/1050001335821585920","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Paleoseismic study on active normal faults in the southeastern Weihe Graben, central China"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002215942220416","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Early Paleozoic tectonic evolution of the North Qinling orogenic belt: Evidence from geochemistry, phase equilibrium modeling and geochronology of metamorphosed mafic rocks from the Songshugou ophiolite"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002218190905984","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Inclination variation in the Late Jurassic to Eocene red beds from southeast Asia: lithological to locality scale approach"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142744332160","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Petrogenesis and Geochronology of Tianshui Granites from Western Qinling Orogen, Central China: Implications for Caledonian and Indosinian Orogenies on the Asian Plate"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182123043328","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tectonic characteristics of the Lishan Piedmont Fault in the SE Weihe Graben (central China), as revealed by the geomorphological and structural analyses"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657453642624","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geomorphological and structural characterization of the southern Weihe Graben, central China: Implications for fault segmentation"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204552882432","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geochronology, geochemistry, and Hf isotopes of the Jiudinggou molybdenum deposit, Central China, and their geological significance"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679527536512","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Single-grain detrital muscovite Rb-Sr isotopic composition as an indicator of provenance for the Carboniferous sedimentary rocks in northern Dabie, China"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679528212864","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"South China provenance of the lower-grade Penglai Group north of the Sulu UHP orogenic belt, eastern China: Evidence from detrital zircon ages and Nd-Hf isotopic composition"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588891962967808","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"ESR signal intensity of quartz in the fine-silt fraction of riverbed sediments from the Yangtze River : a provenance tracer for suspended particulate matter"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/s0040-1951(00)00106-2"},{"@type":"CROSSREF","@value":"10.1111/j.1365-246x.2011.05030.x_references_DOI_RaLLFRnk8DJF9oI74vg5Zfp90UL"},{"@type":"CROSSREF","@value":"10.2343/geochemj.2.0359_references_DOI_RaLLFRnk8DJF9oI74vg5Zfp90UL"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2017.10.024_references_DOI_RaLLFRnk8DJF9oI74vg5Zfp90UL"},{"@type":"CROSSREF","@value":"10.3390/min10060515_references_DOI_RaLLFRnk8DJF9oI74vg5Zfp90UL"},{"@type":"CROSSREF","@value":"10.1186/s40645-017-0118-9_references_DOI_RaLLFRnk8DJF9oI74vg5Zfp90UL"},{"@type":"CROSSREF","@value":"10.2343/geochemj.41.29_references_DOI_RaLLFRnk8DJF9oI74vg5Zfp90UL"},{"@type":"CROSSREF","@value":"10.1016/j.geomorph.2017.01.014_references_DOI_RaLLFRnk8DJF9oI74vg5Zfp90UL"},{"@type":"CROSSREF","@value":"10.2343/geochemj.1.0023_references_DOI_RaLLFRnk8DJF9oI74vg5Zfp90UL"},{"@type":"CROSSREF","@value":"10.1016/j.jseaes.2015.04.031_references_DOI_RaLLFRnk8DJF9oI74vg5Zfp90UL"},{"@type":"CROSSREF","@value":"10.1016/j.gr.2014.10.006_references_DOI_RaLLFRnk8DJF9oI74vg5Zfp90UL"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2014.08.019_references_DOI_RaLLFRnk8DJF9oI74vg5Zfp90UL"}]}