Pangea
Reconstruction of the supercontinent Pangea (or Pangaea) that existed during the late Paleozoic and early Mesozoic eras.
Reconstruction of the supercontinent Pangea (or Pangaea) that existed during the late Paleozoic and early Mesozoic eras.
The Anatolia subduction zone (or ‘Anatolian Neotethys’) started at around 104 Ma as a consequence of fracture zone inversion.
The Oman subduction zone, together with the Anatolian subduction zone, started at around 104 Ma as a consequence of fracture zone inversion.
Global paleogeography with zoomed in figures showing the evolution of oceanic gateways active during the Cenozoic time.