Backarc mantle metasomatized by contrasting types of subducted upper continental crust
One type of mantle-enriching crustal melts had low Zr/Sm and Hf/Sm due to residual zircon.
Depleted and undepleted pre-metasomatic mantle mixed during Pleistocene slab steepening
Three types of mantle sourced Transitional Southern Volcanic Zone arc magmas