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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....
Gorde:
| Argitaratua izan da: | Nat Commun |
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| Egile Nagusiak: | , , |
| Formatua: | Artigo |
| Hizkuntza: | Inglês |
| Argitaratua: |
Nature Publishing Group UK
2021
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| Gaiak: | |
| Sarrera elektronikoa: | 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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