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Paroxysmal eruptions tracked by variations of helium isotopes: inferences from Piton de la Fournaise (La Réunion island)

Helium (He) with its isotopes ((3)He, (4)He) is a key tracer enabling the Earth’s mantle and dynamics to be characterized. Enrichment in primordial helium ((3)He) has been detected in volcanic gases of numerous magmatic systems in different geodynamic settings. Despite past use to monitor volcano-te...

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Detalles Bibliográficos
Autores principales: Boudoire, G., Rizzo, A. L., Arienzo, I., Di Muro, A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7300000/
https://www.ncbi.nlm.nih.gov/pubmed/32555201
http://dx.doi.org/10.1038/s41598-020-66260-x