Tomographic inversion of local earthquake data from the Hengill–Grensdalur central volcano complex
We have determined the three-dimensional P wave velocity structure within the area of the Hengill-Grensdalur central volcano complex, southwest Iceland, from the tomographic inversion of 2409 P wave arrival times recorded by a local earthquake xperiment. The aperture of the 20-element seismic networ...
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| Format: | Text |
| Language: | English |
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1989
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.557.534 http://community.dur.ac.uk/g.r.foulger/Offprints/ToomeyFoulger1989.pdf |