Crustal seismic velocity responds to a magmatic intrusion and seasonal loading in Iceland’s Northern Volcanic Zone

Seismic noise interferometry is an exciting technique for studying volcanoes, providing a continuous measurement of seismic velocity changes (dv/v), which are sensitive to magmatic processes that affect the surrounding crust. However, understanding the exact mechanisms causing changes in dv/v is oft...

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Detalles Bibliográficos
Autores principales: Donaldson, C., Winder, T., Caudron, C., White, R. S.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2019
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6881157/
https://www.ncbi.nlm.nih.gov/pubmed/31807704
http://dx.doi.org/10.1126/sciadv.aax6642

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6881157/
https://www.ncbi.nlm.nih.gov/pubmed/31807704
http://dx.doi.org/10.1126/sciadv.aax6642

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