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.

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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
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Acceso en línea:https://doaj.org/article/9059afb6a9b5462186d7e67751a76706
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