Separating metamorphic events in the Fosdick migmatite–granite complex, West Antarctica

@article{Korhonen2012SeparatingME,
  title={Separating metamorphic events in the Fosdick migmatite–granite complex, West Antarctica},
  author={Fawna J. Korhonen and M. Brown and Marty Grove and Christine Smith Siddoway and Ethan F. Baxter and J. D. Inglis},
  journal={Journal of Metamorphic Geology},
  year={2012},
  volume={30}
}
The Fosdick migmatite–granite complex in West Antarctica records evidence for two high‐temperature metamorphic events, the first during the Devonian–Carboniferous and the second during the Cretaceous. The conditions of each high‐temperature metamorphic event, both of which involved melting and multiple melt‐loss events, are investigated using phase equilibria modelling during successive melt‐loss events, microstructural observations and mineral chemistry. In situ SHRIMP monazite and TIMS Sm–Nd… 

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