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In Contrast To Earlier Hypotheses
The marine Upper Permian and the Permian-Triassic boundary of the Southern Alps between Val Adige (Southern Tyrol, northern Italy) and the Karawanken Mountains (northern Yugoslavia) were studied with respect to microfacies, paleogeography and biostratigraphy. The Upper Permian consists of the Bellerophon Formation (20-360 m thick). The decrease a part of Read more…