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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...

Deskribapen osoa

Gorde:
Xehetasun bibliografikoak
Argitaratua izan da:Nat Commun
Egile Nagusiak: Chiodini, Giovanni, Paonita, Antonio, Aiuppa, Alessandro, Costa, Antonio, Caliro, Stefano, De Martino, Prospero, Acocella, Valerio, Vandemeulebrouck, Jean
Formatua: Artigo
Hizkuntza:Inglês
Argitaratua: Nature Publishing Group 2016
Gaiak:
Sarrera elektronikoa:https://ncbi.nlm.nih.gov/pmc/articles/PMC5187427/
https://ncbi.nlm.nih.gov/pubmed/27996976
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms13712
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