Magmas near the critical degassing pressure drive volcanic unrest towards a critical state

During the reawaking of a volcano, magmas migrating through the shallow crust have to pass through hydrothermal fluids and rocks. The resulting magma–hydrothermal interactions are still poorly understood, which impairs the ability to interpret volcano monitoring signals and perform hazard assessment...

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Detalles Bibliográficos
Autores principales: Chiodini, Giovanni, Paonita, Antonio, Aiuppa, Alessandro, Costa, Antonio, Caliro, Stefano, De Martino, Prospero, Acocella, Valerio, Vandemeulebrouck, Jean
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5187427/
https://www.ncbi.nlm.nih.gov/pubmed/27996976
http://dx.doi.org/10.1038/ncomms13712

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5187427/
https://www.ncbi.nlm.nih.gov/pubmed/27996976
http://dx.doi.org/10.1038/ncomms13712

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