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Figure AF16. Multichannel seismic (MCS) reflection profile (Line CADIZ-21) across the middle slope (CONTOURIBER Project) showing the location of alternate proposed Site GC-10A. Four major low-resolution depositional sequences have been recognized in the Pliocene and Quaternary sedimentary record (Llave et al., 2001; Hernández-Molina et al., 2002, 2006) and are separated by four relevant discontinuities: QBD (base of the Quaternary?) and MPR (mid-Pleistocene?). LPR erosive discontinuity could represent the onset of drift formation. TWT= two-way traveltime.

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