448 KB46 KB200320222003Dozet, Stevoštevilka:2letnik:50str. 525-541ISSN:1408-7073COBISSID_HOST:439902URN:URN:NBN:SI:doc-30G2W2CBenInštitut za rudarstvo, geotehnologijo in okoljeNaravoslovnotehniška fakultetaRMZ-materials and geoenvironmentjuraJurassicOuter Dinaridesstratigrafijastratigrafska vrzelstratigraphySuha krajinaunconformityUpper Triassiczgornji triasZunanji DinaridiMiddle Liassic - Lower Malm stratigraphic gap in Suha krajina| stratigrafska vrzel srednji lias - spodnji malm na območju Suhe krajine|The Upper Triassic and Jurassic stratigraphy as well as the Middle Liassic-Lower Malm stratigraphic gap in the Suha krajina area have been studied in this article. In the cross-section Valicna vas-Sela to the northwest of Žužemberk the Upper Triassic, the Lower and Middle Liassic as well as the Lower and Upper Malm sediments have been recognized. The field and laboratory studies showed that in that part of Slovenia the Upper Liassic and Dogger beds were not deposited. That significant interruption of sedimentary continuity has been caused by intensified epeirogenic movements between the Middle Liassic and the Lower MalmV tem članku so podane zgornjetriasne in jurske stratigrafske razmere ter stratigrafska vrzel srednji lias-spodnji malm na ozemlju Suhe krajine. V profilu Valična vas-Sela severozahodno od Žužemberka so ugotovljeni zgornjetriasni, spodnje- in srednjeliasni ter spodnje- in zgornjemalmski sedimenti. Terensko in laboratorijsko proučevanje je pokazalo, da zgornjeliasne in doggerske plasti v tem delu Slovenije niso bile odložene. To pomembno prekinitev sedimentacije so povzročila pojačana epirogenetska premikanja med srednjim liasom in spodnjim malmomTEXTznanstveno časopisjejournalsSlovenian National E-content AggregatorNational and University Library of SloveniaUniverza v Ljubljani, Naravoslovnotehniška fakulteta