The Magmatic-hydrothermal Transition in Peralkaline Rhyolite Magma at Terceira, Azores
The geochemistry of quartz-hosted melt (MI) and fluid inclusions (FI) in quartz syenite from Terceira, Azores was investigated to provide insight into late-stage evolution of peralkaline melts and the behaviour of high field strength (HFSE) and rare-earth elements (REE) at the magmatic-hydrothermal...
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| Language: | en_ca |
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2014
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| Online Access: | http://hdl.handle.net/1807/65540 |