Estimating the seismotelluric current required for observable electromagnetic ground signals
We use a relatively simple model of an underground current source co-located with the earthquake hypocenter to estimate the magnitude of the seismotelluric current required to produce observable ground signatures. The Alum Rock earthquake of 31 October 2007, is used as an archetype of a typical...
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| Hlavní autoři: | , , , |
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| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Copernicus Publications
2010-08-01
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| Edice: | Annales Geophysicae |
| On-line přístup: | https://www.ann-geophys.net/28/1615/2010/angeo-28-1615-2010.pdf |
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