Page 4 - terraces-chap10
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72 D'ANGELO S. - LEMBO P. - SACCHI L.
ness) of the terrace has been preserved; it's the remnant of erosion at the centre of the profile, in which the same three depositional phase
can be recognized. Regard on this structure only the close is recognizable at about -135 m.
The strong erosion also moves the deposits which cover the bottom of the morphological depression.
