End-Triassic crisis and “unreefing” led to the demise of the Dachstein carbonate platform : A revised model and evidence from the Transdanubian Range, Hungary
The Dachstein platform was an extensive carbonate platform developed on the westernmost shelf of the Neotethys during the Late Triassic, now preserved in various tectonic units disrupted during the Alpine orogeny. Despite being the focus of a multitude of sedimentological, paleontological and other studies, the demise of this platform remains controversial, with contrasting views on the timing and
