Experimental study of the dehydration of 10-Å phase, with implications for its H2O content and stability in subducted lithosphere

The 10-Å phase (TAP) is a hydrous magnesium silicate that forms from the reaction of talc with H 2 O at high pressures. Its high-pressure, low-temperature stability means that it could be a storage site for H 2 O in subduction zones. We have determined the position of the TAP dehydration reaction, T...

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Veröffentlicht in:	Contributions to mineralogy and petrology 2011-12, Vol.162 (6), p.1279-1289
Hauptverfasser:	Pawley, Alison R., Chinnery, Nicholas J., Clark, Simon M., Walter, Michael J.
Format:	Artikel
Sprache:	eng
Schlagworte:	Dehydration Earth and Environmental Science Earth Sciences Geology Geophysics Lithosphere Low temperature Magnesium silicates Mineral Resources Mineralogy Original Paper Petrology Pressure
Online-Zugang:	Volltext
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