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A High Resolution full-field petrophysical model computed using the Geochron approach (Mallet 2004; Moyen & Mallet 2004). The originality of this method lies in the clear separation between the geometric (structural) description of the subsurface and the petrophysical description, which is done in depotitional space. This decoupling between structure and petrophysics offers new perspectives towards better subsurface characterization in complex structural settings.