Hydrous basalt–limestone interaction at crustal conditions: Implications for generation of ultracalcic melts and outflux of CO2 at volcanic arcs

High degassing rates for some volcanoes, typically in continental arcs, (e.g., Colli Albani Volcanic District, Etna, Vesuvius, Italy; Merapi, Indonesia; Popocatepetl, Mexico) are thought to be influenced by magma–carbonate interaction in the crust. In order to constrain the nature of reaction and ex...

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Veröffentlicht in:	Earth and planetary science letters 2015-10, Vol.427, p.202-214
Hauptverfasser:	Carter, Laura B., Dasgupta, Rajdeep
Format:	Artikel
Sprache:	eng
Schlagworte:	arc volcanism Assimilation Basalt Calcite Carbon dioxide Carbonates CO2 degassing Consumption Cylinders experimental petrology limestone assimilation Melts ultracalcic melt inclusions
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