The behaviour of monazite from greenschist facies phyllites to anatectic gneisses: An example from the Chugach Metamorphic Complex, southern Alaska

► Monazite/allanite stability from greenschist-facies phyllites to anatectic gneisses. ► Monazite-in reaction at 540 °C and ≤ 3.4 kbar. ► Dissolution and recrystallisation of monazite during partial melting, 54-51 Ma. ► Destabilisation of monazites related to fault zones.