In the mafic large igneous province formed by plume magmatism, the granites associated with continental flood basalts are non-orogenic, intraplate and A-type granites rather than S-type.

• 地幔柱岩浆作用形成的“镁铁质大火成岩省”中，出现的少量花岗岩是非造山、板内或A-型花岗岩，而不会是S-型花岗岩。