A primary magma is a melt whose composition has not changed since it left its source: it is in equilibrium with the residual mantle, and has neither crystallised minerals nor reacted with the rocks on its way up.
Earth and Space Sciences · Glossary
Earth and Space Sciences · Glossary
A primary magma is a melt whose composition has not changed since it left its source: it is in equilibrium with the residual mantle, and has neither crystallised minerals nor reacted with the rocks on its way up.