Evolución del cabalgamiento de la Muela de Montalbán (Cordillera Ibérica, Teruel)
Three structural units exist in the studied area: the Aliaga basin, the Muela de Montalbán thrust sheet and the Montalbán basin. The former basin is piggy-back on the thrust sheet and the second one is the relative foreland basin. From basin infilling analysis, two evolutionary stages of the thrust...
| Autores: | , , |
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| Formato: | artículo |
| Fecha de publicación: | 1990 |
| País: | España |
| Recursos: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/18171 |
| Acesso em linha: | http://hdl.handle.net/10272/18171 |
| Access Level: | acceso abierto |
| Palavra-chave: | Tectonics and sedimentation Thrust Tertiary Iberian Range |
| Resumo: | Three structural units exist in the studied area: the Aliaga basin, the Muela de Montalbán thrust sheet and the Montalbán basin. The former basin is piggy-back on the thrust sheet and the second one is the relative foreland basin. From basin infilling analysis, two evolutionary stages of the thrust sheet motion are deduced, which gave way to the separation of both basins |
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