Owen Fracture Zone

The Owen Fracture Zone is a transform fault which runs along the eastern boundary of the Arabian Plate, separating it from the Indo-Australian Plate for most of its length, and from the African Plate for a much shorter distance. It extends from the Carlsberg Ridge in the south, meets the Sheba Rift segment of the Aden Ridge, and then continues northeastward across the northwest Indian Ocean until it meets the convergence zone in the Iran-Pakistan border region where the continental crust of the Arabian Plate is colliding with the continental crust of the Eurasian Plate.