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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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| Publicat a: | Nat Commun |
|---|---|
| Autors principals: | , , , , , , , |
| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Nature Publishing Group UK
2018
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| Matèries: | |
| Accés en línia: | 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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