TRENCH
VOLCANIC-MAGMATIC
RANGĘ
Ocean
crust Ocean
scdiments
Sediments eroded from
Subduction melanges: low-temperature, high-pressurc v mctamorphism I
Silicie to mtermedtate mtrusions and lavas: / high-tempecature. / low-pressuro metamorphism i (
Continental
crust
Pcfidotitc melt
Volatilcs and partial melt from subducted ocean płate