Estudio de una transversal entre la cuenca de Madrid y la Cordillera Ibérica a partir de datos estructurales, sísmicos y gravimétricos
An integrated geophysical and geological study has been carried out along a trasverse extending from the Madrid Basin to the Iberian Range. Geological and seismic reflection data were used as background model for the gravity modeling. Mesozoic cover structure is characterized by thrusts, E dipping,...
| Autores: | , , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1995 |
| 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:10272/13489 |
| Acceso en línea: | http://hdl.handle.net/10272/13489 |
| Access Level: | acceso abierto |
| Palabra clave: | Madrid basin Altomira Range Loranca basin Structure Seismic Gravity Forward modeling |
| Sumario: | An integrated geophysical and geological study has been carried out along a trasverse extending from the Madrid Basin to the Iberian Range. Geological and seismic reflection data were used as background model for the gravity modeling. Mesozoic cover structure is characterized by thrusts, E dipping, associated with a decollement located in triassic beds. Gravity modeling shows that high-angle faults bound basement blocks. The faults control triassic sediments thickness |
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