Estructuras paleosísmicas en depósitos h¡dromagmáticos del vulcanismo neógeno del Campo de Calatrava, Ciudad Real (España)
Paleoseismic structures are described for the first time in the volcanism of Campo de Calatrava. The structures are located in hydromagmatic deposits of maars. This study allows to detect seismic activity after the last Quaternary eruptions in the Granatura - Moral Basin (Neogene Age). The liquefied...
| Autores: | , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 2002 |
| País: | España |
| Institución: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/9317 |
| Acceso en línea: | http://hdl.handle.net/10272/9317 |
| Access Level: | acceso abierto |
| Palabra clave: | Seismites Pyroclastic deposits Volcanism Cranátula |
| Sumario: | Paleoseismic structures are described for the first time in the volcanism of Campo de Calatrava. The structures are located in hydromagmatic deposits of maars. This study allows to detect seismic activity after the last Quaternary eruptions in the Granatura - Moral Basin (Neogene Age). The liquefied sediments are conglomerates (lapilli) and the seismic magnitude to liquely this coarse-grained sediment should be higher than 7.5. |
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