Journey to the lower mantle and back
The theory of plate tectonics is at the centre of our understanding of how the Earth works. It has been known for decades that new crust is formed at mid-ocean ridges and that this crust is subducted as plates dive underneath other plates in regions such as the Pacific Ring of Fire and descend into the Earth's mantle. What is not so well known is the fate of these subducted plates.
In this week's edition of the journal Science, scientists from the University of Bristol (Prof. M. Walter, Dr. S. Kohn, Dr. G. Bulanova, Mr. C. Smith), Universidade de Brasilia (Prof. D. Araujo), ...



