{"?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-BSYBDAHT/b2a700f9-52ca-47bc-8f24-d62fa5dd3e08/HTML","dcterms:extent":"50 KB"},{"@rdf:about":"http://www.dlib.si/stream/URN:NBN:SI:DOC-BSYBDAHT/c155e194-cc72-4065-94aa-69459773d20b/PDF","dcterms:extent":"5549 KB"},{"@rdf:about":"http://www.dlib.si/stream/URN:NBN:SI:DOC-BSYBDAHT/23939e77-8606-40f0-889c-483cd60265d3/TEXT","dcterms:extent":"42 KB"}],"edm:TimeSpan":{"@rdf:about":"2000-2024","edm:begin":{"@xml:lang":"en","#text":"2000"},"edm:end":{"@xml:lang":"en","#text":"2024"}},"edm:ProvidedCHO":{"@rdf:about":"URN:NBN:SI:DOC-BSYBDAHT","dcterms:isPartOf":[{"@rdf:resource":"https://www.dlib.si/details/urn:nbn:si:spr-ihg6vo21"},{"@xml:lang":"sl","#text":"Materiali in tehnologije"}],"dcterms:issued":"2010","dc:creator":["Dozet, Stevo","Godec, Matjaž"],"dc:format":[{"@xml:lang":"sl","#text":"številka:4"},{"@xml:lang":"sl","#text":"letnik:44"},{"@xml:lang":"sl","#text":"str. 173-183"}],"dc:identifier":["ISSN:1580-2949","COBISSID:816554","URN:URN:NBN:SI:doc-BSYBDAHT"],"dc:language":"en","dc:publisher":{"@xml:lang":"sl","#text":"Inštitut za kovinske materiale in tehnologije"},"dc:subject":[{"@xml:lang":"sl","#text":"Dinaridi"},{"@xml:lang":"sl","#text":"EDS analiza"},{"@xml:lang":"sl","#text":"elektronska mikroskopija"},{"@xml:lang":"sl","#text":"kaolinit"},{"@xml:lang":"sl","#text":"karbonatne kamnine"},{"@xml:lang":"en","#text":"Slovenia"},{"@xml:lang":"sl","#text":"Slovenija"},{"@xml:lang":"sl","#text":"srednji trias"},{"@xml:lang":"sl","#text":"vulkanske kamnine"},{"@xml:lang":"sl","#text":"XRD"},{"@rdf:resource":"http://www.wikidata.org/entity/Q8042457"}],"dcterms:temporal":{"@rdf:resource":"2000-2024"},"dc:title":{"@xml:lang":"sl","#text":"Middle triassic dry-land phases in southern Slovenia| Srednjetriasne kopenske faze v južni Sloveniji|"},"dc:description":[{"@xml:lang":"sl","#text":"In the Middle Triassic lithostratigraphic sequence of southern Slovenia and neighbouring Gorski Kotar, Croatia, three dry-land phases have been recognized: 1 - between the Lower and Middle Triassic, 2 - in between the Anisian stratigraphic sequence, and 3 - between the Anisian and Ladinian beds. Traces of the Anisian volcanism have also been discovered. The dry-land episodes of the non-deposition and volcanic activity are ascribed to synsedimentary tectonic movements of the Alpine tectonic cycle. However, new data enable a new approach to the paleogeographical evolution of the area. In the Triassic \"Dolomite\" Complex, lenses of kaolinite deposits occur, representing an important correlation horizon for the basal Ladinian beds. They consist chiefly of kaolinite and quartz admixed in smaller quantities by hematite, goethite, nontronite, gibbsite, groutite and montmorillonite. The kaolinite deposits were formed in a marsh with weathering of the pyroclastic materials"},{"@xml:lang":"sl","#text":"V srednjetriasnem litostratigrafskem zaporedju južne Slovenije in sosednjega Gorskega Kotarja (Hrvaška) so ugotovljene tri okopnitve, in sicer: 1 - med spodnjim in srednjim triasom, 2 - v aniziju ter 3 - med anizijem in ladinijem. Odkriti so tudi sledovi anizijskega vulkanizma. Okopnitve in vulkanizem povezujemo s sočasnimi tektonskimi premiki Alpidskega tektonskega cikla. Novi podatki omogočajo nov pogled na paleogeografski razvoj obravnavanega ozemlja. V triasnem dolomitnem kompleksu se pojavljajo leče kaolinitnih usedlin, ki so pomemben korelacijski horizont za bazalne ladinijske plasti. Sestojijo v glavnem iz kaolinita in kremena, katerima so v manjših količinah primešani hematit, goethit, nontronit, gibbsit, groutit in montomorilonit. Kaolinitne usedline so nastale v močvirju pri razpadu piroklastičanega materiala"}],"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-BSYBDAHT","edm:aggregatedCHO":{"@rdf:resource":"URN:NBN:SI:DOC-BSYBDAHT"},"edm:isShownBy":{"@rdf:resource":"http://www.dlib.si/stream/URN:NBN:SI:DOC-BSYBDAHT/c155e194-cc72-4065-94aa-69459773d20b/PDF"},"edm:rights":{"@rdf:resource":"http://rightsstatements.org/vocab/InC/1.0/"},"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":"Inštitut za kovinske materiale in tehnologije"},"edm:object":{"@rdf:resource":"http://www.dlib.si/streamdb/URN:NBN:SI:DOC-BSYBDAHT/maxi/edm"},"edm:isShownAt":{"@rdf:resource":"http://www.dlib.si/details/URN:NBN:SI:DOC-BSYBDAHT"}}}}