Cargando…
Transient to stationary radon ((220)Rn) emissions from a phonolitic rock exposed to subvolcanic temperatures
Rock substrates beneath active volcanoes are frequently subjected to temperature changes caused by the input of new magma from the depth and/or the intrusion of magma bodies of variable thickness within the subvolcanic rocks. The primary effect of the influx of hot magma is the heating of surroundin...
| Autores principales: | , , , , , |
|---|---|
| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
The Royal Society
2019
|
| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6837235/ https://www.ncbi.nlm.nih.gov/pubmed/31824701 http://dx.doi.org/10.1098/rsos.190782 |