A study of rare earth element (REE)–SiO2 variations in felsic liquids generated by basalt fractionation and amphibolite melting: a potential test for discriminating between the two different processes
The origin of felsic magmas (>63% SiO 2 ) in intra-oceanic arc settings is still a matter of debate. Two very different processes are currently invoked to explain their origin. These include fractional crystallization of basaltic magma and partial melting of lower crustal amphibolite. Because bot...
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Veröffentlicht in: | Contributions to mineralogy and petrology 2008-09, Vol.156 (3), p.337-357 |
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