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Role of syn-eruptive plagioclase disequilibrium crystallization in basaltic magma ascent dynamics

Timescales of magma ascent in conduit models are typically assumed to be much longer than crystallization and gas exsolution for basaltic eruptions. However, it is now recognized that basaltic magmas may rise fast enough for disequilibrium processes to play a key role on the ascent dynamics. The qua...

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Detalles Bibliográficos
Autores principales: La Spina, G., Burton, M., de' Michieli Vitturi, M., Arzilli, F.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5159818/
https://www.ncbi.nlm.nih.gov/pubmed/27941750
http://dx.doi.org/10.1038/ncomms13402