Abstract
Paleomagnetic studies of sediments from the Calabro-Peloritan block in
southern Italy consequently imply a 15° clockwise rotation for the late Tortonian to
middle Pleistocene sedimentary cover; but the results of older sediments are
generally less consistent. Earlier paleomagnetic results of Tortonian sites from the
Basilicoi section (Crotone basin, northern Calabria) suggested a major
counterclockwise rotation
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