Fig. 8.
Variation diagrams showing components that partition into the residuum: (a) (Na2O+CaO) and (b) (MgO + FeOT) vs K2O, a component that partitions into anatectic melt. Note that some leucodiatexites and leucogranites contain more K2O than the field of anatectic melts. In (a) the AMM plots just above the pink field because its composition has been adjusted to be compatible with Archean metagreywacke (see text).