What defines the boundary between the Earth's lithosphere and asthenosphere? Here it is shown experimentally that the instability of the hydrous mineral pargasite at depths greater than about 90 km causes a sharp drop in the water-storage capacity of a fertile upper-mantle mineralogy, and accordingly a sharp drop in its solidus temperate. This effect might define the lithosphere–asthenosphere boundary.
- David H. Green
- William O. Hibberson
- Anja Rosenthal
