Article ID Journal Published Year Pages File Type
6440986 Lithos 2012 15 Pages PDF
Abstract
► 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.
Keywords
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geochemistry and Petrology
Preview
The behaviour of monazite from greenschist facies phyllites to anatectic gneisses: An example from the Chugach Metamorphic Complex, southern Alaska
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