Figure 6
From: An updated reconstruction of basaltic crust emplacement in Tyrrhenian sea, Italy
Stratigraphy of ODP Site 651 (Vavilov plain). (A) Main litho-stratigraphic units; the lower unit consists of complex igneous basement which has serpentinized peridotite at the bottom, whereas sediments of LmP and Pleistocene age form the upper unit. (B) Line drawing of the seismic reflection profile ST12 crossing drill-site on east flank of basement swell (see text). Location of seismic reflection profile is indicated in Fig. 4.
