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R. Catalano et al. j Tectonophysics 260 ( /996) 291-323      305

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Fig. 14. Maghrebian-Sicilian Inner Carbonate TS. NW-SE-trending seismic profile shows, between 8 and 5 s (t.w.t.), some strong
reflectors interpreted as carbonate platfonn tops of deeper thrust which underlie duplexes of interpreted basin type rocks and tectonic slices
of terrigenous deposits (Numidian or equivalent Aysch roof-complex) (modified after Catalano et al., 1993b and Sulli, 1994). Plio-Pieisto-
cene sediments partly cover the Messinian (M) reflector. FN- Numidian Aysch; Tb - top of basinal successions; Tp - top of platfonn
carbonates. Location of the seismic profile in Fig. IO.
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