Abstract
Abstract Tertiary gravity sliding of the north Calabrian sedimentary series in Italy is considered with reference to a system of large displacement thrust faults, and to facies change between western siliceous sediments and eastern reef sediments. The eastward sliding of the nappe is traced until it collided with the north Calabrian massifs and was split. One part slid onto the coastal chain and central Calabria; the other pushed the Calabro-Lucanian massifs east and then north.
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