La deformación intraplaca del centro de España y la interpretación de los perfiles profundos de sísmica de reflexión en las Cordilleras Béticas
The interpretation of the ESCI-Béticas deep seismic reflection profiles allows to define the type of deformation in the suture zone of the Iberian-Alborân crustal domains in the central Betics. This suture zone corresponds to a crustal thrust that accommodated shortening in its footwall block along...
| Autores: | , , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1994 |
| 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:10272/13994 |
| Acceso en línea: | http://hdl.handle.net/10272/13994 |
| Access Level: | acceso abierto |
| Palabra clave: | Deep seismic reflection profiles Crustal shortening Intraplate stress transmissio Central Betics Spanish Central System |
| Sumario: | The interpretation of the ESCI-Béticas deep seismic reflection profiles allows to define the type of deformation in the suture zone of the Iberian-Alborân crustal domains in the central Betics. This suture zone corresponds to a crustal thrust that accommodated shortening in its footwall block along the cover (Subbetics)-basement (Hercynian crust) detachment. This fact and the absence of a true continental hypercollision, lead to discard the existence of a mid-crustal detachment whose emersion caused the formation of the Spanish Central System |
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