{"@context":{"dc":"http:\/\/purl.org\/dc\/elements\/1.1\/","skos":"http:\/\/www.w3.org\/2004\/02\/skos\/core#","skos:broader":{"@type":"@id"},"skos:inScheme":{"@type":"@id"},"skos:related":{"@type":"@id"},"skos:narrower":{"@type":"@id"},"skos:hasTopConcept":{"@type":"@id"},"skos:topConceptOf":{"@type":"@id"}},"@id":"https:\/\/confrides.cpd.ua.es\/tematres\/vocab\/skos\/3863","@type":"skos:Concept","skos:prefLabel":{"@language":"es","@value=":"Sedimentos marinos"},"skos:inScheme":"https:\/\/confrides.cpd.ua.es\/tematres\/vocab\/","dct:created":"2009-05-25 13:27:49","skos:scopeNote":[{"@lang":null,"@value":"Bajo este encabezamiento se encuentran las obras que tratan de los restos minerales y \u00f3rganicos del actual fondo submarino. Las obras que tratan de los sedimentos minerales y org\u00e1nicos situados en tierras emergidas en la actualidad se encuentran bajo el encabezamiento Sedimentos (Geolog\u00eda). Se subdivide por lugares, p. ej.: Sedimentos marinos - M\u00e9xico, Golfo de; Sedimentos marinos - Pac\u00edfico, Costa del "},{"@lang":"es","@value":"Se puede usar con un subencabezamiento geogr\u00e1fico. "}],"skos:historyNote":[{"@lang":"es","@value":"Revisada el 13 de noviembre de 2019 "}],"skos:note":[{"@lang":"es","@value":"CDU: 551.35\nCDU: 551.462 "},{"@lang":"es","@value":"Fuente: Suplem. USE "}],"skos:broader":["https:\/\/confrides.cpd.ua.es\/tematres\/vocab\/skos\/3830"],"skos:altLabel":[{"language":"es","value":"Dep\u00f3sitos marinos"},{"language":"es","value":"Dep\u00f3sitos pel\u00e1gicos"},{"language":"es","value":"Sedimentos abisales"},{"language":"es","value":"Sedimentos pel\u00e1gicos"},{"language":"es","value":"Terrenos pel\u00e1gicos"}],"skos:related":["https:\/\/confrides.cpd.ua.es\/tematres\/vocab\/skos\/1213","https:\/\/confrides.cpd.ua.es\/tematres\/vocab\/skos\/3869","https:\/\/confrides.cpd.ua.es\/tematres\/vocab\/skos\/4031","https:\/\/confrides.cpd.ua.es\/tematres\/vocab\/skos\/3870","https:\/\/confrides.cpd.ua.es\/tematres\/vocab\/skos\/3862"]}