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Initially, researchers attempted to show that one or the other of these process acted exclusively to cause magmatic differentiation.
With historical perspective, we now realize that if any of them are possible, then any or all of these processes could act at the same time to produce chemical change, and thus combinations of these processes are possible.
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If all of the liquid is removed, then we have the case of fractional melting, which is somewhat different.
In fractional melting all of the liquid is removed at each stage of the process.
In such a case each magma might represent melting of a different source rock at different times during the heating event.
If this were the case, we might not expect the chemical analyses of the rocks produced to show smooth trends on variation diagrams.