Fig. 11
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Isochrone maps (in TWTT seconds) of the main Pliocene-Pleistocene units in the Provençal Basin. (a) The MSC-P11 TWTT-thickness (5.33-2.6 Ma) map corresponds to the salt tectonics phase 2, characterized by the formation of the listric faults in the extensional domain. (b) Q10-SB (0.9-0 Ma) TWTT-thickness map corresponds to the youngest part of the salt tectonics phase 3 described in this work, characterized by an intense deformation and orientation of the salt structures in the present-day Rhône thalweg direction. The profiles are shown in Figures 8, 9 and 10.
Cartes isochrones (en secondes TWTT) des principales unités pliocènes-pléistocènes dans le Bassin Provençal. a) La carte d’épaisseur TWTT du MSC-P11 (5,33-2,6 Ma) correspond à la phase 2 de la tectonique salifère. b) La carte d’épaisseur TWTT du Q10-SB (0,9-0 Ma) correspond à la partie la plus récente de la phase 3 de la tectonique salifère décrite dans ce travail.
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