{"@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/1363670320982335232.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1007/978-1-4615-5935-1"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1007/978-1-4615-5935-1.pdf"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1007/978-1-4615-5935-1"}}],"dc:title":[{"@value":"Tectonic Uplift and Climate Change"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380285532879684867","@type":"Researcher","foaf:name":[{"@value":"WF Ruddiman"}]}],"contributor":[{"@id":"https://cir.nii.ac.jp/crid/1383670320982335232","@type":"Researcher","foaf:name":[{"@value":"William F. Ruddiman"}],"role":"editor"}],"publication":{"publicationIdentifier":[{"@type":"ISBN","@value":"9781461377191"},{"@type":"ISBN","@value":"9781461559351"}],"dc:publisher":[{"@value":"Springer US"}],"prism:publicationDate":"1997"},"reviewed":"false","dc:rights":["http://www.springer.com/tdm"],"url":[{"@id":"http://link.springer.com/content/pdf/10.1007/978-1-4615-5935-1.pdf"},{"@id":"http://link.springer.com/content/pdf/10.1007/978-1-4615-5935-1"}],"createdAt":"2011-07-26","modifiedAt":"2020-01-29","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360848662554980224","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The turnover of continental planktonic diatoms near the middle/late Miocene boundary and their Cenozoic evolution"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204061379072","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Paleoenvironment and climate changes caused by the Himalayan Tectonics in the East Asia"},{"@language":"ja","@value":"ヒマラヤ山脈のテクトニクスと東アジアの古環境・古気候の変動"},{"@language":"ja-Kana","@value":"ヒマラヤ サンミャク ノ テクトニクス ト ヒガシアジア ノ コ カンキョウ コ キコウ ノ ヘンドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679206497024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Evolution of Large Scale Topography and Variation in Climate"},{"@language":"ja","@value":"大地形の変遷と気候変動"},{"@language":"ja-Kana","@value":"ダイチケイ ノ ヘンセン ト キコウ ヘンドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681214999168","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Climate model simulation on the role of mountain uplift on Asian monsoon"},{"@language":"ja","@value":"チベット高原の隆起がアジアモンスーンに及ぼす影響に関する気候モデルシミュレーション"},{"@language":"ja-Kana","@value":"チベット コウゲン ノ リュウキ ガ アジアモンスーン ニ オヨボス エイキョウ ニ カンスル キコウ モデル シミュレーション"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151841908060032","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evolution and variability of the Asian monsoon and its potential linkage with uplift of the Himalaya and Tibetan Plateau"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1007/978-1-4615-5935-1"},{"@type":"CROSSREF","@value":"10.5026/jgeography.117.1015_references_DOI_9jBrQ3Rmf9oon9YmUtr5TstUD6g"},{"@type":"CROSSREF","@value":"10.1186/s40645-016-0080-y_references_DOI_9jBrQ3Rmf9oon9YmUtr5TstUD6g"},{"@type":"CROSSREF","@value":"10.3720/japt.70.6_references_DOI_9jBrQ3Rmf9oon9YmUtr5TstUD6g"},{"@type":"CROSSREF","@value":"10.1371/journal.pone.0198003_references_DOI_9jBrQ3Rmf9oon9YmUtr5TstUD6g"},{"@type":"CROSSREF","@value":"10.5575/geosoc.111.654_references_DOI_9jBrQ3Rmf9oon9YmUtr5TstUD6g"}]}