{"?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-LV4IIZJQ/10d3806b-225d-4dff-ba8f-9ddd911643cd/PDF","dcterms:extent":"2184 KB"},{"@rdf:about":"http://www.dlib.si/stream/URN:NBN:SI:doc-LV4IIZJQ/4b9fec61-e2f4-4816-bdf7-3a6e11578db0/TEXT","dcterms:extent":"15 KB"}],"edm:TimeSpan":{"@rdf:about":"1954-2025","edm:begin":{"@xml:lang":"en","#text":"1954"},"edm:end":{"@xml:lang":"en","#text":"2025"}},"edm:ProvidedCHO":{"@rdf:about":"URN:NBN:SI:doc-LV4IIZJQ","dcterms:isPartOf":[{"@rdf:resource":"https://www.dlib.si/details/URN:NBN:SI:spr-B4L2ESHC"},{"@xml:lang":"sl","#text":"Geografski obzornik"}],"dcterms:issued":"1997","dc:creator":"Kunaver, Jurij","dc:format":[{"@xml:lang":"sl","#text":"številka:3"},{"@xml:lang":"sl","#text":"letnik:44"},{"@xml:lang":"sl","#text":"str. 11-18"}],"dc:identifier":["ISSN:0016-7274","COBISSID:3938402","URN:URN:NBN:SI:doc-LV4IIZJQ"],"dc:language":"sl","dc:publisher":{"@xml:lang":"sl","#text":"Zveza geografskih društev Slovenije"},"dc:subject":[{"@xml:lang":"sl","#text":"Francija"},{"@xml:lang":"sl","#text":"geografija"},{"@xml:lang":"sl","#text":"geotektonika"},{"@xml:lang":"sl","#text":"Nemčija"},{"@xml:lang":"sl","#text":"Ren"},{"@xml:lang":"sl","#text":"tektonski premiki"}],"dcterms:temporal":{"@rdf:resource":"1954-2025"},"dc:title":{"@xml:lang":"sl","#text":"O nastanku in pomenu renskega tektonskega jarka in sosedstva|"},"dc:description":[{"@xml:lang":"sl","#text":"The Rhine Rift valley shape is the result of the rifting which begins some 60 milion years ago. It is known as a hot spot due to the eruption of the hot mantle into the crust, which caused the crust uplift and the mantle overflow with the development of the Black Forest, the Vosges and the Rhine Rift valley. The region discussed is the most important European traffic corridor which has great economic potential"},{"@xml:lang":"sl","#text":"Renski tektonski jarek je posledica že več kot 60 milijonov let trajajočega vdora stebra plaščne magme v zemeljsko skorjo, znanega pod imenom vroča točka. Povzročil je dviganje in razmikanje Schwarzwalda in Vogezov ter nastanek tektonskega jarka med njima. Kot osrednja evropska prometna os med severno in južno Evropo ima jarek tudi pomembno gospodarsko vlogo"}],"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-LV4IIZJQ","edm:aggregatedCHO":{"@rdf:resource":"URN:NBN:SI:doc-LV4IIZJQ"},"edm:isShownBy":{"@rdf:resource":"http://www.dlib.si/stream/URN:NBN:SI:doc-LV4IIZJQ/10d3806b-225d-4dff-ba8f-9ddd911643cd/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":"Zveza geografov Slovenije"},"edm:object":{"@rdf:resource":"http://www.dlib.si/streamdb/URN:NBN:SI:doc-LV4IIZJQ/maxi/edm"},"edm:isShownAt":{"@rdf:resource":"http://www.dlib.si/details/URN:NBN:SI:doc-LV4IIZJQ"}}}}