U-Th-Ba Elemental Fractionation during Partial Melting of Crustal Xenoliths and its Implications for U-series Disequilibria in Continental Arc Rocks
Understanding U-series isotopic disequilibria of partially melted crust is integral for determining the effect that crustal assimilation has on the U-series signature of magmas. In this work, U, Th and Ba (as a proxy for Ra) elemental abundances were gathered on the quenched glass in partially melt...
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| Format: | Others |
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FIU Digital Commons
2011
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| Online Access: | http://digitalcommons.fiu.edu/etd/406 http://digitalcommons.fiu.edu/cgi/viewcontent.cgi?article=1458&context=etd |