Evolution of Plinian magmas from Popocatépetl Volcano, México
Fractional crystallization, magma mixing, assimilation of continental crust, and how those processes modify volatile budgets, control the evolution of magma. As a consequence, the understanding of these processes, their magnitudes, and timescales is critical for interpreting ancient magma systems, t...
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| Format: | Others |
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2014
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| Online Access: | http://hdl.handle.net/2152/ETD-UT-2011-08-3928 http://hdl.handle.net/2152/26905 |