{"@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/1360292621244487808.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.3402/tellusa.v10i1.9223"}},{"identifier":{"@type":"URI","@value":"https://account.a.tellusjournals.se/index.php/su-j-tadmo/article/download/3575/6705"}}],"dc:title":[{"@value":"Quartz Contents of Pelagic Sediments of the Pacific Ocean"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The quartz contents of pelagic clays from the Eastern Pacific Ocean show a marked latitudinal dependence with a maximum around 30°N. Present evidence indicates that the quartz is mainly transported to the deposits through the atmosphere and that the observed distribution is probably related to the latitudinal values of the atmospheric wind fluxes and exposed arid land areas. A number of sediments display a distinct change in quartz content with depth. In all cases there is a marked decrease going from the recent to the older strata. It is suggested that the changes indicate a major climatic change that occured sometime during the Late Tertiary.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380292621244487808","@type":"Researcher","foaf:name":[{"@value":"Robert W. Rex"}]},{"@id":"https://cir.nii.ac.jp/crid/1380292621244487809","@type":"Researcher","foaf:name":[{"@value":"Edward D. Goldberg"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"16000870"}],"prism:publicationName":[{"@value":"Tellus A: Dynamic Meteorology and Oceanography"}],"dc:publisher":[{"@value":"Stockholm University Press"}],"prism:publicationDate":"1958-01-01","prism:volume":"10","prism:number":"1","prism:startingPage":"153","prism:endingPage":"159"},"reviewed":"false","dc:rights":["https://creativecommons.org/licenses/by/4.0"],"url":[{"@id":"https://account.a.tellusjournals.se/index.php/su-j-tadmo/article/download/3575/6705"}],"createdAt":"2012-01-20","modifiedAt":"2025-10-16","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360588379383159168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Linearity of natural versus laboratory-imparted remanence demagnetization diagram and reliability of relative paleointensity estimation"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206564051584","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Mercury concentration in the ocean."},{"@language":"ja","@value":"海洋の水銀濃度"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681480233728","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"春季北太平洋西部海域における海上大気中のエーロゾル粒子の化学成分の変動について"},{"@language":"en","@value":"Effect of the Continental Dust Over the North Pacific Ocean: Time Variation of Chemical Components in Maritime"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681542442624","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Seasonal and areal variation of continental aerosol in the surface air over the western North Pacific region."},{"@language":"ja","@value":"西部北太平洋域表層大気中の大陸起源エーロゾルの季節的・地域的変動"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317019149312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Rock magnetism of quartz and feldspars chemically separated from pelagic red clay : a new approach to provenance study"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317028457600","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Unmixing biogenic and terrigenous magnetic mineral components in red clay of the Pacific Ocean using principal component analyses of first-order reversal curve diagrams and paleoenvironmental implications"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.3402/tellusa.v10i1.9223"},{"@type":"CROSSREF","@value":"10.2151/jmsj1965.61.4_670_references_DOI_UU7QJwNOto7p3hFvkdmxWqkaZka"},{"@type":"CROSSREF","@value":"10.1186/s40623-020-01248-5_references_DOI_UU7QJwNOto7p3hFvkdmxWqkaZka"},{"@type":"CROSSREF","@value":"10.1186/s40623-025-02140-w_references_DOI_UU7QJwNOto7p3hFvkdmxWqkaZka"},{"@type":"CROSSREF","@value":"10.1186/s40623-018-0918-1_references_DOI_UU7QJwNOto7p3hFvkdmxWqkaZka"},{"@type":"CROSSREF","@value":"10.1007/bf02109036_references_DOI_UU7QJwNOto7p3hFvkdmxWqkaZka"},{"@type":"CROSSREF","@value":"10.1007/bf02071824_references_DOI_UU7QJwNOto7p3hFvkdmxWqkaZka"}]}