Oman ophiolite suggests subduction started with a shove
Oman ophiolite suggests subduction started with a shove by Mary Caperton Morton Friday, December 21, 2018 Past research has suggested two mechanisms by which subduction zones may form along an area of lithospheric weakness: spontaneous sinking of denser crust and lithosphere, and forced convergence driven by lateral movement of a plate. A new study suggests that the latter was responsible for the formation of a fossil subduction zone off the Arabian Peninsula beginning about 104 million years ago. Credit: K. Cantner, AGI. Plate tectonics is a fundamental control on how Earth operates...