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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| Автори: | , , , |
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| Формат: | Artigo |
| Мова: | Inglês |
| Опубліковано: |
Copernicus Publications
2010-08-01
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| Серія: | Annales Geophysicae |
| Онлайн доступ: | https://www.ann-geophys.net/28/1615/2010/angeo-28-1615-2010.pdf |
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