{"?xml":{"@version":"1.0"},"edm:RDF":{"@xmlns:dc":"http://purl.org/dc/elements/1.1/","@xmlns:edm":"http://www.europeana.eu/schemas/edm/","@xmlns:wgs84_pos":"http://www.w3.org/2003/01/geo/wgs84_pos","@xmlns:foaf":"http://xmlns.com/foaf/0.1/","@xmlns:rdaGr2":"http://rdvocab.info/ElementsGr2","@xmlns:oai":"http://www.openarchives.org/OAI/2.0/","@xmlns:owl":"http://www.w3.org/2002/07/owl#","@xmlns:rdf":"http://www.w3.org/1999/02/22-rdf-syntax-ns#","@xmlns:ore":"http://www.openarchives.org/ore/terms/","@xmlns:skos":"http://www.w3.org/2004/02/skos/core#","@xmlns:dcterms":"http://purl.org/dc/terms/","edm:WebResource":[{"@rdf:about":"http://www.dlib.si/stream/URN:NBN:SI:doc-FUTNZ7VA/2c76e918-ccfd-4e3d-9195-2107bf144c1b/HTML","dcterms:extent":"10 KB"},{"@rdf:about":"http://www.dlib.si/stream/URN:NBN:SI:doc-FUTNZ7VA/6c83bca2-c5eb-4ea1-a826-f8d3eec177cb/PDF","dcterms:extent":"139 KB"},{"@rdf:about":"http://www.dlib.si/stream/URN:NBN:SI:doc-FUTNZ7VA/af457323-7538-4376-9bd3-78502c4184fe/TEXT","dcterms:extent":"5 KB"}],"edm:TimeSpan":{"@rdf:about":"1953-2025","edm:begin":{"@xml:lang":"en","#text":"1953"},"edm:end":{"@xml:lang":"en","#text":"2025"}},"edm:ProvidedCHO":{"@rdf:about":"URN:NBN:SI:doc-FUTNZ7VA","dcterms:isPartOf":[{"@rdf:resource":"https://www.dlib.si/details/URN:NBN:SI:spr-Y5SOGFOQ"},{"@xml:lang":"sl","#text":"Geologija"}],"dcterms:issued":"2000","dc:creator":["Grad, Karel","Kralj, Polona"],"dc:format":[{"@xml:lang":"sl","#text":"številka:2"},{"@xml:lang":"sl","#text":"4 strani"},{"@xml:lang":"sl","#text":"letnik:knj. 43"},{"@xml:lang":"sl","#text":"str. 219-221"}],"dc:identifier":["ISSN:0016-7789","COBISSID:700245","URN:URN:NBN:SI:doc-FUTNZ7VA"],"dc:language":"en","dc:publisher":{"@xml:lang":"sl","#text":"Geološki zavod Slovenije"},"dc:subject":[{"@xml:lang":"sl","#text":"Domžale"},{"@xml:lang":"sl","#text":"klastične kamnine"},{"@xml:lang":"sl","#text":"oligocen"},{"@xml:lang":"sl","#text":"predornine"},{"@xml:lang":"sl","#text":"vulkanske kamnine"}],"dcterms:temporal":{"@rdf:resource":"1953-2025"},"dc:title":{"@xml:lang":"sl","#text":"Oligocene tuffs at Domžale, the Ljubljana basin, Slovenia|"},"dc:description":[{"@xml:lang":"sl","#text":"Oligocene volcanics have not been found yet in the Ljubljana basin. At Domžale, fine-grained tuffs predominate, although coarse-grained and lapilli tuffs also occur. The main constituents are volcanic glass shards. The tuffs are rhyolitic in composition. Alteration is reflected in the development of clay minerals - calcic montmorillonite and illite"},{"@xml:lang":"sl","#text":"V ljubljanski kotlini do sedaj še nismo našli predornin oligocenske starosti. Pri Domžalah prevladujejo drobnozrnati tufi, med njimi pa se pojavljajo tudi debelozrnati in lapilni tufi. Glavna sestavina tufov so črepinjice vulkanskegastekla. Sestava tufov je riolitna. Spremembe se odražajo predvsem vkristalizaciji glinenih mineralov - kalcijskega montmorillonita in illita"}],"edm:type":"TEXT","dc:type":[{"@xml:lang":"sl","#text":"znanstveno časopisje"},{"@xml:lang":"en","#text":"journals"},{"@rdf:resource":"http://www.wikidata.org/entity/Q361785"}]},"ore:Aggregation":{"@rdf:about":"http://www.dlib.si/?URN=URN:NBN:SI:doc-FUTNZ7VA","edm:aggregatedCHO":{"@rdf:resource":"URN:NBN:SI:doc-FUTNZ7VA"},"edm:isShownBy":{"@rdf:resource":"http://www.dlib.si/stream/URN:NBN:SI:doc-FUTNZ7VA/6c83bca2-c5eb-4ea1-a826-f8d3eec177cb/PDF"},"edm:rights":{"@rdf:resource":"http://creativecommons.org/licenses/by/4.0/"},"edm:provider":"Slovenian National E-content Aggregator","edm:intermediateProvider":{"@xml:lang":"en","#text":"National and University Library of Slovenia"},"edm:dataProvider":{"@xml:lang":"sl","#text":"Geološki zavod Slovenije"},"edm:object":{"@rdf:resource":"http://www.dlib.si/streamdb/URN:NBN:SI:doc-FUTNZ7VA/maxi/edm"},"edm:isShownAt":{"@rdf:resource":"http://www.dlib.si/details/URN:NBN:SI:doc-FUTNZ7VA"}}}}