Abstract
Abstract The correlation of carbonate platform and slope sediments with biostratigraphically and radiometrically dated basinal successions in the Western Dolomites allows the reconstruction of the growth of a Middle Triassic carbonate platform (Schlern/Rosengarten) over a time interval of approximately five ammonoid zones (Reitzi, Secedensis, Curionii, Gredleri, Archelaus zones). The whole platform evolution had a total duration of
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