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...

Ful tanımlama

Kaydedildi:
Detaylı Bibliyografya
Yayımlandı:Nat Commun
Asıl Yazarlar: Wadsworth, Fabian B., Witcher, Taylor, Vossen, Caron E. J., Hess, Kai-Uwe, Unwin, Holly E., Scheu, Bettina, Castro, Jonathan M., Dingwell, Donald B.
Materyal Türü: Artigo
Dil:Inglês
Baskı/Yayın Bilgisi: Nature Publishing Group UK 2018
Konular:
Article
Online Erişim: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
Etiketler: Etiketle
Etiket eklenmemiş, İlk siz ekleyin!

Benzer Materyaller