Fig. 6: The Alboran Ridge Fault System (ARFS) depth structure and evolution models. | Nature Communications

Fig. 6: The Alboran Ridge Fault System (ARFS) depth structure and evolution models.

From: Evidence for a developing plate boundary in the western Mediterranean

Fig. 6

Pre-stack depth migrated section across the Alboran Ridge (see Figs. 1 and 2 for location). The crustal dimension of the ARFS is inferred for the different reflectivity observed on the two sides of the fault, together with the different Moho depths (black dots). AIFS: Al-Idrissi Fault System, M: Messinian unconformity, vD: volcanics Djibouti Plateau, vAR: volcanics Alboran Ridge.

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