Crystals reveal magma convection and melt transport in dyke-fed eruptions

The processes and ranges of intensive variables that control magma transport and dyke propagation through the crust are poorly understood. Here we show that textural and compositional data of olivine crystals (Mg/Fe, Ni and P) from the tephra of the first months of Paricutin volcano monogenetic erup...

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Detalles Bibliográficos
Autores principales: Albert, Helena, Larrea, Patricia, Costa, Fidel, Widom, Elisabeth, Siebe, Claus
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7363826/
https://www.ncbi.nlm.nih.gov/pubmed/32669582
http://dx.doi.org/10.1038/s41598-020-68421-4

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7363826/
https://www.ncbi.nlm.nih.gov/pubmed/32669582
http://dx.doi.org/10.1038/s41598-020-68421-4

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