Fig. 6.

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Geological sections of the Sibari basin. #1 and #2 are normal faults. For the depth conversion of Pleistocene and Messinian seismic units we assumed, respectively an average V p of 2000 and 3000 m/s.
Geological sections of the Sibari basin. #1 and #2 are normal faults. For the depth conversion of Pleistocene and Messinian seismic units we assumed, respectively an average V p of 2000 and 3000 m/s.
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