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...
Published in: | Science Advances |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
AAAAS
2019
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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 |