{"?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-0O3NES5F/45befc98-c16e-4ffc-9d3f-27790cfa9dfe/HTML","dcterms:extent":"40 KB"},{"@rdf:about":"http://www.dlib.si/stream/URN:NBN:SI:doc-0O3NES5F/dd2bc9e7-d6f0-49f5-8181-952551cb7665/PDF","dcterms:extent":"133 KB"},{"@rdf:about":"http://www.dlib.si/stream/URN:NBN:SI:doc-0O3NES5F/cb5619d8-ea4a-4917-80c9-af89a247e60b/TEXT","dcterms:extent":"38 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-0O3NES5F","dcterms:isPartOf":[{"@rdf:resource":"https://www.dlib.si/details/URN:NBN:SI:spr-Y5SOGFOQ"},{"@xml:lang":"sl","#text":"Geologija"}],"dcterms:issued":"2004","dc:creator":"Celarc, Bogomir","dc:format":[{"@xml:lang":"sl","#text":"11 strani"},{"@xml:lang":"sl","#text":"številka:2"},{"@xml:lang":"sl","#text":"letnik:knj. 47"},{"@xml:lang":"sl","#text":"str. 139-149"}],"dc:identifier":["ISSN:0016-7789","COBISSID:1103445","URN:URN:NBN:SI:doc-0O3NES5F"],"dc:language":"sl","dc:publisher":{"@xml:lang":"sl","#text":"Geološki zavod Slovenije"},"dc:subject":[{"@xml:lang":"sl","#text":"apnenec"},{"@xml:lang":"sl","#text":"dolomit"},{"@xml:lang":"en","#text":"Kamnik–Savinja Alps"},{"@xml:lang":"sl","#text":"Kamniško-Savinjske Alpe"},{"@xml:lang":"sl","#text":"karbonatne kamnine"},{"@xml:lang":"en","#text":"Slovenia"},{"@xml:lang":"sl","#text":"Slovenija"},{"@xml:lang":"sl","#text":"stratigrafija"},{"@xml:lang":"en","#text":"stratigraphy"},{"@xml:lang":"sl","#text":"trias"}],"dcterms:temporal":{"@rdf:resource":"1953-2025"},"dc:title":{"@xml:lang":"sl","#text":"Problematika \"cordevolskih\" apnencev in dolomitov v slovenskih Južnih Alpah| Problems of the \"Cordevolian\" limestone and dolomite in the Slovenian part of the Southern Alps|"},"dc:description":[{"@xml:lang":"sl","#text":"Stratigraphic position and age of the so called Cordevolian limestone and dolomite in the Slovenian part of the Southern Alps is a long lasting problem.Its name originates from the (somewhere abandoned) Cordevolian substage (Lower Carnian). Limestone and dolomite both correspond to the Cassian dolomite from the Italian Southern Alps. Platform type of limestone and dolomite, which could be genetic and time equivalent with the Ladinian Schlern (Scilliar) dolomite, is unknown in Slovenia. In the NE part of the Kamnik-Savinja Alps, the Korošica formation (Upper Ladinian) overlies platformlimestone and dolomite of the Ojstrica Formation (Ladinian). Diploporaannulata is also present in the Ojstrica formation. Various Ladinian rocks in the Julian Alps and Southern Karavanke are mainly of the Lover Ladinian age, whereas the overlying massive limestone and dolomite (\"Cordevolian limestone and dolomite\") are partially of the Ladinian and partially of the Carnian age. There are no Upper Ladinian \"Wengen\" beds in thecarbonate massive, so it is impossible to draw a time line between the Ladinian and the Carnian stages. We can therefore conclude, that litological boundaries do not coincide with the chronostratigraphic ones"},{"@xml:lang":"sl","#text":"V slovenskih Južnih Alpah je problematična stratigrafska uvrstitev in starost t. i. cordevolskega apnenca in dolomita, ki so ju slovenski raziskovalci poimenovali po cordevolski podstopnji karnija, ki jo ponekod več ne uporabljajo. Apnenci in dolomiti naj bi ustrezali cassianskemu dolomitu iz italijanskih Južnih Alp. V slovenskih Južnih Alpah ne poznamo platformnih grebenskih apnencev in dolomitov ladinijske starosti, ki bi bili časovni in genetski ekvivalent schlernskega dolomita. V severovzhodnemu delu Kamniško - Savinjskih Alp leži Korošiška formacija (zgornji del ladinija) na platformskihapnencih in dolomitih Ojstriške formacije, ki je ladinijske starosti. V apnencih najdemo tudi algo Diplopora annulata. Za preučevanje triasne stratigrafije Julijskih Alp in Južnih Karavank se torej odpira zanimiva problematika, zato na podlagi literaturnih podatkov podajam predlog stratigrafske razvrstitve posameznih litoloških enot, saj menim, da so različne kamnine, ki jim raziskovalci pripisujejo celoten ladinijski razpon, pretežno spodnjeladinijske starosti, masivni apnenci in dolomiti nad njimi pa so deloma ladinijske in deloma karnijske starosti. V karbonatnem masivu ne najdemo horizonta zgornjeladinijskih \"wengenskih\" plasti, ki bi predstavljal značilen, sledljiv horizont, tako da ne moremo postaviti meje med ladinijem inkarnijem. Litološke meje se v tem primeru ne ujemajo s kronostratigrafskimi"}],"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-0O3NES5F","edm:aggregatedCHO":{"@rdf:resource":"URN:NBN:SI:doc-0O3NES5F"},"edm:isShownBy":{"@rdf:resource":"http://www.dlib.si/stream/URN:NBN:SI:doc-0O3NES5F/dd2bc9e7-d6f0-49f5-8181-952551cb7665/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-0O3NES5F/maxi/edm"},"edm:isShownAt":{"@rdf:resource":"http://www.dlib.si/details/URN:NBN:SI:doc-0O3NES5F"}}}}