Depositional environment of the Middle Triassic Strelovec Formation on Mt. Raduha, Kamnik-Savinja Alps, northern SloveniaMiklavc, Primož (Avtor) Celarc, Bogomir (Avtor) Southern Alpsbituminous limestonesrestricted basinintraformational brecciaAnisianfacies analysisThe Raduha section represents a continuation of the research of the Anisian Strelovec Formation in the Kamnik-Savinja Alps. The Strelovec Formation was deposited during the Anisian on a drowned section of the Serla Dolomite carbonate platform in a restricted probably outer ramp environment associated with an intraplatform basin. The base of the section is represented by dolostone breccia containing angular carbonate lithoclasts of shallow-marine origin. This is followed by alternations of laminated and homogenous hemipelagic limestones deposited in a restricted and anoxic environment. Hemipelagic sedimentation was occasionally interrupted by clay input and deposition of sediments from gravity mass flows. Slow filling of the basin lead to a gradual cessation of anoxic conditions and sedimentation of bedded shallow-marine limestones. After shallow water conditions were established, bioclastic dolostone of the Contrin Formation was deposited.Geološki zavod Slovenije20222023-01-18 10:04:02Neznano16085UDK: 55ISSN pri članku: 0016-7789DOI: 10.5474/geologija.2022.014COBISS_ID: 135260419sl