The 1998-1999 eruption of Volcán de Colima, Mexico: an application of Maeda's viscoelastic model
A modified version of Maeda's viscoelastic model of mass ejection is applied to the 1998-1999 eruptive period of Volcán de Colima, Mexico. The model fits reasonably well the observed volume and volume rate of the eruption, assuming a magma chamber with a volume 30 km3 and radius of 1.93 km centered...
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| Vydáno v: | Geofísica Internacional |
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| Hlavní autoři: | , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Universidad Nacional Autónoma de México
2010
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| Témata: | |
| On-line přístup: | https://www.redalyc.org/articulo.oa?id=56819044004 |
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