Estructuras paleosísmicas en depósitos hidromagmáticos del vulcanismo neógeno del Campo de Calatrava, Ciudad Real (España)
Paleoseismic structures are described far 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 Complutense de Madrid (UCM) |
| Repositorio: | Docta Complutense |
| Idioma: | español |
| OAI Identifier: | oai:docta.ucm.es:20.500.14352/58092 |
| Acceso en línea: | https://hdl.handle.net/20.500.14352/58092 |
| Access Level: | acceso abierto |
| Palabra clave: | 551.21 Seismites Pyroclastic deposits Volcanism Granátula Geodinámica 2507 Geofísica |
| Sumario: | Paleoseismic structures are described far 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 fiquely this coarse-grained sediment should be higher than 7.5. |
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