OUC Made New Progress on Redox Cycling in Subduction Zones
Subduction is a key process that controls the redox state of the mantle, arc magma formation, and the evolution of Earth’s oxidation state. However, whether and how subducting slabs transport oxidized material to the sub-arc and back-arc mantle has long been intensely debated. Recently, Professor Li Sanzhong of Ocean University of China (OUC), together with Dr. Duan Wenyong, a postdoctoral researcher at Swiss Federal Institute of Technology (ETH Zurich), and other scholars from China and abroad,