Satellite radar interferometry 1993-1999 suggests deep accumulation of magma near the crust-mantle boundary at the Krafla volcanic system, Iceland
Author:
Affiliation:
1. Volcano Dynamics Group, Department of Earth Sciences; The Open University; Milton Keynes UK
2. Nordic Volcanological Institute; University of Iceland; Reykjavik Iceland
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Reference18 articles.
1. Sources of crustal deformation associated with the Krafla, Iceland, eruption of September 1984;Árnadóttir;Geophys. Res. Lett.,1998
2. Färoe-Iceland ridge experiment: 2. Crustal structure of the Krafla central volcano;Brandsdóttir;J. Geophys. Res.,1997
3. Estimating source parameters from deformation data, with an application to the March 1997 earthquake swarm off the Izu Peninsula, Japan;Cervelli;J. Geophys. Res.,2001
4. Post-rifting stress-relaxation at the divergent plate boundary in northeast Iceland;Foulger;Nature,1992
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