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This rock would begin to melt at the peritectic point, where Di, En, Ol, and Liquid are in equilibrium.The composition of the liquid would remain at the peritectic point (labeled 0% melting) until all of the diopside melted. The liquid would then take a path shown by the dark curve, first moving along the En - Ol boundary curve, until the enstatite was completely absorbed, then moving in a direct path toward the peridotite composition.Initially, researchers attempted to show that one or the other of these process acted exclusively to cause magmatic differentiation.
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This liquid will have the same composition as pure Forsterite ("Melt 3").(Note that the compositions between 0% melting and where the dark line intersects the En-Di join are Si Oundersaturated liquids).
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