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Reconciling bubble nucleation in explosive eruptions with geospeedometers
Magma from Plinian volcanic eruptions contains an extraordinarily large numbers of bubbles. Nucleation of those bubbles occurs because pressure decreases as magma rises to the surface. As a consequence, dissolved magmatic volatiles, such as water, become supersaturated and cause bubbles to nucleate....
Wedi'i Gadw mewn:
| Cyhoeddwyd yn: | Nat Commun |
|---|---|
| Prif Awduron: | , , |
| Fformat: | Artigo |
| Iaith: | Inglês |
| Cyhoeddwyd: |
Nature Publishing Group UK
2021
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| Pynciau: | |
| Mynediad Ar-lein: | https://ncbi.nlm.nih.gov/pmc/articles/PMC7803785/ https://ncbi.nlm.nih.gov/pubmed/33436589 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-020-20541-1 |
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