Decoding polyphase migmatites using geochronology and phase equilibria modelling
In this study, in situ U–Pb monazite ages and Lu–Hf garnet geochronology are used to distinguish mineral parageneses developed during Devonian–Carboniferous and Cretaceous events in migmatitic paragneiss and orthogneiss from the Fosdick migmatite–granite complex in West Antarctica. SHRIMP U–Pb monaz...
| Main Authors: | , , , , , , , |
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| Format: | Journal Article |
| Published: |
Blackwell Publishing Inc.
2015
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| Online Access: | http://hdl.handle.net/20.500.11937/46610 |