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A palaeomagnetic study of late Early Miocene to late Middle Miocene sediments from the Eastern Alpine intramontane basins revealed counterclockwise rotations in the Ennstal, in the western part of the Noric and in the Lavanttal depressions. For the basal strata of the basins, declinations are between 273 o and 315 o , while for the younger strata they are between 321 o and...
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