Stable isotope (18 O/16 O and D/H) studies of cascade volcanic arc magmatism
Stable isotope ratios (¹⁸ O/¹⁶ O and D/H) potentially constrain origins of magma and volatile sources in igneous rocks. Modification of magmas by closed system processes (fractional crystallization and closed system devolatilization) or open-syst...
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| Language: | en |
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2009
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| Online Access: | http://etd.lib.montana.edu/etd/2009/underwood/UnderwoodS0809.pdf |