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Fingerprint of silicic magma degassing visualised through chlorine microscopy

Volatile-rich silicic magma erupts either explosively as a jet of a mixture of pyroclasts and high-temperature gas, or non-explosively to effuse lava. The bifurcation of the eruption style is widely recognised as being controlled by the efficiency of open-system gas loss from vesiculated magma durin...

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Detalles Bibliográficos
Autores principales: Yoshimura, Shumpei, Kuritani, Takeshi, Matsumoto, Akiko, Nakagawa, Mitsuhiro
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6349900/
https://www.ncbi.nlm.nih.gov/pubmed/30692567
http://dx.doi.org/10.1038/s41598-018-37374-0

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