Crystal plasticity as an indicator of the viscous-brittle transition in magmas
The rheological behaviour of magma in shallow conditions may help determine a volcano’s eruptive style. Here, the authors perform deformation experiments on lava from Volcán de Colima to demonstrate that crystal plasticity may preclude failure at certain shallow magmatic conditions.
Guardado en:
Autores principales: | J. E. Kendrick, Y. Lavallée, E. Mariani, D. B. Dingwell, J. Wheeler, N. R. Varley |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2017
|
Materias: | |
Acceso en línea: | https://doaj.org/article/9059afb6a9b5462186d7e67751a76706 |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
Ejemplares similares
-
Combined effusive-explosive silicic volcanism straddles the multiphase viscous-to-brittle transition
por: Fabian B. Wadsworth, et al.
Publicado: (2018) -
The influence of the brittle-ductile transition zone on aftershock and foreshock occurrence
por: Giuseppe Petrillo, et al.
Publicado: (2020) -
A laboratory study of hydraulic fracturing at the brittle-ductile transition
por: Francesco Parisio, et al.
Publicado: (2021) -
Generalization of intrinsic ductile-to-brittle criteria by Pugh and Pettifor for materials with a cubic crystal structure
por: O. N. Senkov, et al.
Publicado: (2021) -
Ductile and brittle transition behavior of titanium alloys in ultra-precision machining
por: W. S. Yip, et al.
Publicado: (2018)