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...

Disgrifiad llawn

Wedi'i Gadw mewn:
Manylion Llyfryddiaeth
Cyhoeddwyd yn:Nat Commun
Prif Awduron: Wadsworth, Fabian B., Witcher, Taylor, Vossen, Caron E. J., Hess, Kai-Uwe, Unwin, Holly E., Scheu, Bettina, Castro, Jonathan M., Dingwell, Donald B.
Fformat: Artigo
Iaith:Inglês
Cyhoeddwyd: Nature Publishing Group UK 2018
Pynciau:
Article
Mynediad Ar-lein:https://ncbi.nlm.nih.gov/pmc/articles/PMC6224499/
https://ncbi.nlm.nih.gov/pubmed/30409969
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-018-07187-w
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