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Vesicle shrinkage in hydrous phonolitic melt during cooling
The ascent of hydrous magma prior to volcanic eruptions is largely driven by the formation of H(2)O vesicles and their subsequent growth upon further decompression. Porosity controls buoyancy as well as vesicle coalescence and percolation, and is important when identifying the differences between eq...
| Autores principales: | , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Springer Berlin Heidelberg
2020
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7080310/ https://www.ncbi.nlm.nih.gov/pubmed/32214430 http://dx.doi.org/10.1007/s00410-020-1658-3 |