Quantitative field constraints on the dynamics of silicic magma chamber rejuvenation and overturn
A number of recent papers by Bachmann and co-authors investigate a hypothesis that the catastrophic eruption of large-volume, crystal-rich silicic magmas is a consequence of reheating (so-called rejuvenation) and overturn of partially molten, buoyant silicic material by repeated injection of dense,...
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| Language: | English |
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University of British Columbia
2010
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| Online Access: | http://hdl.handle.net/2429/27430 |
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