20.500.12556/DiRROS-19208 Middle Triassic deeper-marine volcano-sedimentary successions in western Slovenia Srednjetriasna globljemorska vulkansko-sedimentna zaporedja v zahodni Slovenij A Ladinian – Carnian volcano-sedimentary succession from western Slovenia, paleogeographically belonging to the western Slovenian Basin, is presented in 17 sections. Except for the lowermost part, which is dominated by volcanics and volcaniclastics, most of the succession is dominated by shale, sandstone, and micritic limestone. Various authors use the name Pseudozilja and/or Amphiclina formation for this part, which is dominated by clastics, but they disagree on the differences between the formations. The lower Pseudozilja formation, represented by the Malenski Vrh section, comprises diabase, tuf and shale. No substantial differences in lithological composition have been observed between the upper Pseudoziljaformation and the Amphiclina formation, which are predominantly composed of shale, sandstone, and limestone. The shale and sandstone are largely composed of quartz, feldspar, and lithic grains (especially volcanics), which vary in proportions. Limestone varieties comprise hemipelagic limestones and resedimented carbonates deposited by gravity-flows. Deposition of the Ladinian – Carnian volcano-sedimentary succession took place on or near the continental slope that was generally inclined to the S, with the direction of transport mainly from N to S. V članku v 17 profilih predstavljamo ladinijsko – karnijsko vulkansko-sedimentno zaporedje zahodne Slovenije, paleogeografsko umeščeno v zahodni del Slovenskega bazena. Spodnji del psevdoziljske formacije, posnet na Melenskem vrhu, sestavljajo diabaz, tuf in laminiran muljevec. Zgornji del psevdoziljske formacije in amfiklinska formacija sta litološko identična. V večjem delu ju sestavljajo laminiran muljevec, peščenjak in apnenec. Glavne sestavine muljevca in peščenjaka so kremen, glinenci in litična zrna (predvsem predornin) v različnih razmerjih. Apnenec obsega hemipelagični apnenec in resedimentirane karbonate. Sedimentacija ladinijsko – karnijskega vulkansko-sedimentnega zaporedja je potekala na ali v bližini kontinentalnega pobočja z nagibom proti jugu. Transport sedimenta je v glavnem potekal od severa proti jugu. stratigraphy carbonate-siliciclastic deposits Slovenian Basin Middle Triassic Ladinian Carnian Pseudozilja formation Amphiclina formation stratigrafija karbonatno-siliciklastični sediment Slovenski bazen srednji trias ladinij karnij psevdoziljska formacija amfiklinska formacija true false true Geološki zavod Slovenije Angleški jezik Slovenski jezik Neznano 2024-07-09 08:36:21 2024-07-09 08:36:21 2024-07-10 03:52:50 0000-00-00 00:00:00 2024 0 0 str. 71-103 no. 1 vol. 67 2024 0000-00-00 Zaloznikova Objavljeno NiDoloceno 0000-00-00 0000-00-00 2024-06-11 55 0016-7789 10.5474/geologija.2024.005 198945283 1885-Article_Text-12342542-1-10-20240611.pdf 1885-Article_Text-12342542-1-10-20240611.pdf 1 D1468D11E62EAB4388BAE57F71EDC2D0 7a63a08cc8f401fb94b372de29238b04ae390e4f64d701436b9b241e01f61ab1 0a8e13fc-3dbe-11ef-b487-001a4af901a5 https://dirros.openscience.si/Dokument.php?lang=slv&id=26444 Geološki zavod Slovenije Geologija 0 0 0