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Fingerprint of silicic magma degassing visualised through chlorine microscopy
Volatile-rich silicic magma erupts either explosively as a jet of a mixture of pyroclasts and high-temperature gas, or non-explosively to effuse lava. The bifurcation of the eruption style is widely recognised as being controlled by the efficiency of open-system gas loss from vesiculated magma durin...
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| Vydáno v: | Sci Rep |
|---|---|
| Hlavní autoři: | , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Nature Publishing Group UK
2019
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6349900/ https://ncbi.nlm.nih.gov/pubmed/30692567 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-018-37374-0 |
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