Combined effusive-explosive silicic volcanism straddles the multiphase viscous-to-brittle transition

Magma is a viscoelastic fluid that can support fracture propagation when local shear stresses are high, or relax and flow when shear stresses are low. Here we present experiments to confirm this using synthetic and natural magmatic liquids across eruptive conditions and use Maxwell’s linear viscoela...

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Detalles Bibliográficos
Autores principales: Wadsworth, Fabian B., Witcher, Taylor, Vossen, Caron E. J., Hess, Kai-Uwe, Unwin, Holly E., Scheu, Bettina, Castro, Jonathan M., Dingwell, Donald B.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6224499/
https://www.ncbi.nlm.nih.gov/pubmed/30409969
http://dx.doi.org/10.1038/s41467-018-07187-w

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6224499/
https://www.ncbi.nlm.nih.gov/pubmed/30409969
http://dx.doi.org/10.1038/s41467-018-07187-w

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