45 KB1758 KB42 KB195320252000Dozet, StevoStrohmenger, Christian16 straništevilka:2letnik:knj. 43str. 197-212ISSN:0016-7789COBISSID:699733URN:URN:NBN:SI:doc-P4PUQFDHslGeološki zavod SlovenijeGeologijaapnenecdolomitjurasedimentistratigrafijastratigraphyPodbukovška formacija, osrednja Slovenija|Detailed geological mapping as well as stratimetric measurement and sedimentological investigations have been performed in the Suha Krajina area. On the basis of facies analysis of several cross-sectionsin the considered area the lithostratigraphic and biostratigraphic subdivision of the Lower Jurassic stratigraphic sequence has been carried out. Lying without any discordance upon the Main dolomite (Hauptdolomit) and being slightly discordantly overlain by the Laze formation (Hočevje group), the considered stratigraphic interval consists exclusively of carbonate rocks. The successionof carbonate rocks lying between the Main dolomite and Laze formation has been designated as Podbukovje formation. The formation consists of 5 lithostratigraphic members and two biozones belonging to the LiassicNa območju Suhe krajine je na podlagi nadrobne facijalne analize sedimentov izvedena litostratigrafska in biostratigrafska analiza plasti spodnjejurske skladovnie. Sedimentno zaporedje, ki leži konkordantno na Glavnem dolomitu, rahlo diskordantno na njej pa plasti formacije Laze (Hočevska skupina), sestavljajo izključno apnenci in dolomiti. Označeno je z imenom Podbukovška formacija. Sestoji iz petih litostratigrafskih enot in dveh biostratigrafskih biocon liasne starostiTEXTznanstveno časopisjejournalsSlovenian National E-content AggregatorNational and University Library of SloveniaGeološki zavod Slovenije