The Gulf of Lion is not a simple continental margin; it results from Oligocene-Miocene anti-clockwise rotation of the Corsican-Sardinian Block against the European Craton.
I-Bay of León ayisiwo umngcele olula wezwekazi, kodwa umphumela weqembu i-Oligocene-Miocene Corsican-Sardinian eligijima liphikisana nse ne-Europa Craton.