The volatile contents of melt inclusions and implications for mantle degassing and ocean island evolution
The amount of volatile elements dissolved in silicate melts is a controlling factor in a range of geologic processes, which include hazardous volcanic eruptions, economically-significant ore-forming systems, and global-scale volatile fluxes, which contribute to planetary evolution. While melt volati...
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Virginia Tech
2019
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| Online Access: | http://hdl.handle.net/10919/93345 |