Estudio de una transversa entre la cuenca de Madrid y la Cordillera Ibérica a partir de datos estructurales, sísmicos y gravimétricos
An integrated gheophysical and geological study has been carried out along a transverse extending from the Madrid Basin to the Iberian Range. Geological and seismic reflection data were used as background nodel for the gravity modeling. Mesozoic cover structure is characterized by thruss, E dipping...
| Autores: | , , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1995 |
| País: | España |
| Institución: | Universidad Complutense de Madrid (UCM) |
| Repositorio: | Docta Complutense |
| Idioma: | español |
| OAI Identifier: | oai:docta.ucm.es:20.500.14352/56920 |
| Acceso en línea: | https://hdl.handle.net/20.500.14352/56920 |
| Access Level: | acceso abierto |
| Palabra clave: | Madrid basin Altomira Range Loranca basin Structure Seismic Gravity Forward modeling Geodinámica 2507 Geofísica |
| Sumario: | An integrated gheophysical and geological study has been carried out along a transverse extending from the Madrid Basin to the Iberian Range. Geological and seismic reflection data were used as background nodel for the gravity modeling. Mesozoic cover structure is characterized by thruss, E dipping associated with a decollement located in triassic beds. Gravity modeling shows that high-angle faults bound basement blocks. The faults control triassic sediment thickness. |
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