{"@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/1364233270931563264.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/jd094id15p18379"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2FJD094iD15p18379"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/JD094iD15p18379"}}],"dc:title":[{"@value":"Late Cenozoic uplift in southern Asia and the American West: Rationale for general circulation modeling experiments"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Geologic evidence suggests significant increases in uplift rates and absolute elevation in several areas during the late Cenozoic, especially in the last 10 m.y. Regions of major uplift include the Tibetan Plateau and Himalayan Mountains of southern Asia; and the Sierra Nevada, Colorado Plateau, Basin and Range, Rocky Mountains, and High Plains of the American west. Uplift occurred at a scale large enough to affect regional and global climate in a number of ways, several of which we evaluate by General Circulation Model experiments in accompanying papers.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380285532879684764","@type":"Researcher","foaf:name":[{"@value":"W. F. Ruddiman"}]},{"@id":"https://cir.nii.ac.jp/crid/1384233270931563264","@type":"Researcher","foaf:name":[{"@value":"W. L. Prell"}]},{"@id":"https://cir.nii.ac.jp/crid/1384233270931563266","@type":"Researcher","foaf:name":[{"@value":"M. E. Raymo"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"},{"@type":"PISSN","@value":"https://id.crossref.org/issn/01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Atmospheres"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1989-12-20","prism:volume":"94","prism:number":"D15","prism:startingPage":"18379","prism:endingPage":"18391"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2FJD094iD15p18379"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/JD094iD15p18379"}],"createdAt":"2008-02-06","modifiedAt":"2023-09-22","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360567182369840512","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stable carbon isotopic variation of long chain n-alkanoic acids in the equatorial Pacific sediments over the last 40Ma: Implications for expansion of C4 grassland in South America"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206238319872","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Terrestrial Cosmogenic Nuclides as a tool for studying earth surface processes"},{"@language":"ja","@value":"宇宙線照射生成核種を用いた地球表層プロセスの研究"},{"@language":"ja-Kana","@value":"ウチュウセン ショウシャ セイセイカクシュ オ モチイタ チキュウ ヒョウソウ プロセス ノ ケンキュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206502063616","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Effects of Large-Scale Mountains on Surface Climate. 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