We use Cretaceous faults sub-perpendicular to the NAF-N as precise offset markers.
We provide a robust estimate of 52 ± 1 km displacement along the major NAF-N.
We propose a total of ~ 88 ± 5 km offset along all branches of the NAF in Marmara Sea.
Our data suggest Pliocene (3.9 Ma) inception age for the NAF in the Marmara region.
We interpret that the Marmara Basins opened as transtensional structures.