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- W147035243 abstract "The evolution of the overall structure can be then divided in two different steps: 1)the onset of subsidence started in the Late Miocene and covered a large areas presently occupied by the Paola and Crotone basins. This basin, was probably already separated into sub-basins but evolved in a slowly subsiding and poorly deformed area located between the active accretionary prism and the volcanic arc. Therefore in the Middle-Upper Miocene this basin could be defined as forearc basin. 2)In the Pliocene the structure of this large basin was fragmented due to the uplift of a central range (Sila Massif) with an overall pop-up like structure. 3)Uplift of the belt producing subsidence along the flanks and simultaneously formation of two distinct basins: the Paola and Crotone basins. This process probably occurred during episodes of fast roll-back of the subducting slab, as attested by the opening of two ocean floor basins in the back-arc region." @default.
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- W147035243 date "2009-04-01" @default.
- W147035243 modified "2023-09-28" @default.
- W147035243 title "Neogene to Quaternary evolution of the Calabrian Subduction System, (Central Mediterranean)" @default.
- W147035243 hasPublicationYear "2009" @default.
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