Crystallisation in basaltic magmas revealed via in situ 4D synchrotron X-ray microtomography

Magma crystallisation is a fundamental process driving eruptions and controlling the style of volcanic activity. Crystal nucleation delay, heterogeneous and homogeneous nucleation and crystal growth are all time-dependent processes, however, there is a paucity of real-time experimental data on cryst...

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Detalles Bibliográficos
Autores principales: Polacci, M., Arzilli, F., La Spina, G., Le Gall, N., Cai, B., Hartley, M. E., Di Genova, D., Vo, N. T., Nonni, S., Atwood, R. C., Llewellin, E. W., Lee, P. D., Burton, M. R.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5976632/
https://www.ncbi.nlm.nih.gov/pubmed/29849174
http://dx.doi.org/10.1038/s41598-018-26644-6

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5976632/
https://www.ncbi.nlm.nih.gov/pubmed/29849174
http://dx.doi.org/10.1038/s41598-018-26644-6

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