The La Veteada Formation, in the Sierra de Famatina (west of Argentina), is one few records Early Triassic age South America verified by isotopic and palynological assemblages. This unit composed sandstones, mudstones, shales, limestones, marls, with some levels gypsum, chert, tuff levels. In its stratotype, Formation rests on Late Permian red beds Talampaya covered Neogene breccias conglomerat...