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deposited from slackwater fallout and deposited on the top of the Tournaisian unit. Fig. 4. Sedimentary structures of estuary/lagoon depositional environment in the transgressive cycle A: microlaminated mudstone and siltstone with horizontal and wavy
Permian), regional subsidence resulted in thick continental sediments. From the Middle–Late Permian, the sediment accumulation was influenced by a regional transgression. The sea-level rise changed the type of sedimentation (Late Permian): above the
western part of the Tethys Ocean ( Fig. 2 ). The Mesozoic sedimentary cycle as preserved in the TDR began with a latest Paleozoic transgression. By the end of the Triassic an extensive, coherent, few km-thick Dachstein-type platform developed ( Haas, 1988
Tournaisian reefal and other carbonate facies. A cyclic transgressive-regressive marine deposition took place following the Tournaisian, producing a thick interfingering nearshore deltaic/interdeltaic marine and continental-coastal clastic sequence. The
et al., 1999a ) which is Badenian in age ( Kelemen et al., 2021 ); kaolinite deposition was partly coeval with marine sediments of the grabens around the KH ( Fodor et al., 2021 ). The transgression of Lake Pannon reached the area of the KH
,261 ± 52 cal BP (4,364–4,260 BC), i.e., at the beginning of the Copper Age ( Raczky 1988 , 1995 ; Vaday 2004 ; Szilágyi 2008 ). The transition of the late Neolithic and Copper Ages was a time-transgressive process ( Gyucha et al. 2004 , 2006
Olenekian ( Szulc 1999 , 2000 ), and the westernmost communication to the Tethys was effective during the Anisian ( Feist-Burkhardt et al. 2008a ; Götz and Gast 2010 ). Major transgressive phases are recognized by phytoplankton peaks ( Götz and Feist
the Pannonian Basin with diverse sedimentary environments ( Lučić et al. 2001 ) at the onset of marine transgression during the Middle Badenian ( Ćorić et al. 2009 ). In the well Tek-1, the Vukovar formation is represented by a mixed section of coarse
., BOULIS , S. N . , 2012 . Glauconites from the Bahariya Oasis: an evidence for Cenomanian marine transgression in Egypt . Journal of African Earth Sciences . 70 . 1 – 7 . BAIOUMY , H. M ., BOULIS , S. N ., HASSAN , M. S . , 2012 . Occurrences
2004 : Roggendorf-1 borehole, a key section for lower Badenian transgressions and the stratigraphic position of the Grund Formation (Molasse Basin, Lower Austria) . – Geologica Carpatica , 55 , pp. 165 – 178
