Ultra-high pressure metamorphism

Related publications

Structural, Petrological and Chemical Analysis of Syn-Kinematic Migmatites: Insights from the Western Gneiss Region, Norway.
Ganzhorn, A. C., L. Labrousse, G. Prouteau, C. Leroy, J. C. Vrijmoed, T. B. Andersen, and L. Arbaret (2014)
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Metasomatism in the Ultrahigh-Pressure Svartberget Garnet-Peridotite (Western Gneiss Region, Norway): Implications for the Transport of Crust-Derived Fluids within the Mantle.
Vrijmoed, J. C., H. Austrheim, T. John, R. C. Hin, F. Corfu, and G. R. Davies (2013)
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An alternative model for ultra-high pressure in the Svartberget Fe-Ti garnet-peridotite, Western Gneiss Region, Norway.
Vrijmoed, Johannes C., Yuri Y. Podladchikov, Torgeir B. Andersen, and Ebbe H. Hartz, (2009)
European Journal of Mineralogy 21 (6): 1119-33. doi:10.1127/0935-1221/2009/0021-1985.

Raman confirmation of microdiamond in the Svartberget Fe-Ti type garnet peridotite, Western Gneiss Region, Western Norway.
Vrijmoed, J. C., D. C. Smith, and H. L. M. van Roermund, (2008)
Terra Nova 20 (4): 295-301. doi:10.1111/j.1365-3121.2008.00820.x.

Evidence for diamond-grade ultra-high pressure metamorphism and fluid interaction in the Svartberget Fe-Ti garnet peridotite-websterite body, Western Gneiss Region, Norway.
Vrijmoed, J. C., H. L. M. Van Roermund, and G. R. Davies, (2006)
Mineralogy and Petrology 88 (1-2): 381-405. doi:10.1007/s00710-006-0160-6.