Timing Vapor–Melt Equilibration in Silicic Magmas
Magmas experiencing pressure changes can follow equilibrium or nonequilibrium degassing paths that determine the rate of gas exsolution and the composition of gases exsolved. Many variables influence timescales of equilibration between vapor and melt after a perturbation in pressure, temperature, or...
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| Language: | en_US |
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University of Oregon
2017
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| Online Access: | http://hdl.handle.net/1794/22717 |