Resumé
Glacial earthquakes are slow slip-events located under major outlet glaciers. These peculiar events were first discovered by Ekstrom et al in 2003 using teleseismic data and a global detection algorithm based on surface waves. The waveforms are consistent with a landslide-type focal mechanism, thus indicating that the seismological signals are linked to glacier movements.
| Originalsprog | Engelsk |
|---|---|
| Artikelnummer | EGU2007-A-03541 |
| Antal sider | 1 |
| Tidsskrift | Geophysical Research Abstracts |
| Vol/bind | 9 |
| Status | Udgivet - 2007 |
| Begivenhed | EGU General Assembly 2007 - Vienna, Austria Varighed: 16 apr. 2007 → 20 apr. 2007 |
Programområde
- Programområde 3: Energiressourcer