The distribution of rare earth elements between monzogranitic melt and the aqueous volatile phase in experimental investigations at 800 degrees C and 200 MPa
The partitioning of the rare earth elements between a peraluminous monzogranitic melt and a chloride-bearing, sulfur- and carbon dioxide-free, aqueous volatile phase was examined experimentally as a function of chloride and major element concentrations at 800 degreesC and 200 MPa. The light rare ear...
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Veröffentlicht in: | Contributions to mineralogy and petrology 2000-12, Vol.140 (2), p.251 |
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Sprache: | eng |
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