Estimation of Relative Seismic Velocity Changes Around Katla Volcano, Using Coda in Ambient Seismic Noise
Relative seismic velocity variations in the Earth’s crust can be estimated by using ambient seismic noise records from a pair of stations. Velocity variations can be caused by stress perturbations in the subsurface. Therefore, information on stress changes in the crust can possibly be retrieved from...
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Format: | Others |
Language: | English |
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Uppsala universitet, Institutionen för geovetenskaper
2018
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Online Access: | http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-353619 |