Subsidencia sísmica en las cuencas neógenas lacustres del Prebético de Albacete
Seismic subsidence has been calculated in the Prebetic Neogene basins of Albacete (Betic Chain, Spain). The existent paleoseismic data allow us to know the number of earthquakes and their approximate magnitudes. The paleoseismic events are located into varved beds therefore we has obtained the sedim...
| Autores: | , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 2000 |
| País: | España |
| Institución: | Universidad Complutense de Madrid (UCM) |
| Repositorio: | Docta Complutense |
| Idioma: | español |
| OAI Identifier: | oai:docta.ucm.es:20.500.14352/57973 |
| Acceso en línea: | https://hdl.handle.net/20.500.14352/57973 |
| Access Level: | acceso abierto |
| Palabra clave: | 550.34 Seismic subsidence Lacustrine basins Paleoseismic data Sismología (Geología) 2507.05 Sismología y Prospección Sísmica |
| Sumario: | Seismic subsidence has been calculated in the Prebetic Neogene basins of Albacete (Betic Chain, Spain). The existent paleoseismic data allow us to know the number of earthquakes and their approximate magnitudes. The paleoseismic events are located into varved beds therefore we has obtained the sedimentation rate. Using rupture parameters in faults (rupture length and surface displacement) we has calculated the seismic subsidence rate, in base of the sedimentation rate The minimum seismic subsidence value is 10% and 50% as maximum. |
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