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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Bibliographic Details
Published in:Science Advances
Main Authors: Donaldson, Clare, Winder, Tom, Caudron, Corentin, White, Robert S.
Format: Article in Journal/Newspaper
Language:unknown
Published: AAAAS 2019
Subjects:
Online Access:http://eprints.esc.cam.ac.uk/4513/
https://advances.sciencemag.org/content/5/11/eaax6642.full
https://doi.org/10.1126/sciadv.aax6642