Grandes fallas de contracción y de extensión implicadas en el contacto entre los dominios de Alborán y Sudibérico en el arco de Gibraltar
Constitutive units of Alboran and Sudiberic Domains near Gibraltar Arc are specified. The boundary between both domains results from a crustal scale westward transpressive thrust and superimposed Iow angle normal faults later developed. Thus most of the tectonic contacts presently observed are exten...
| Autores: | , |
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| Formato: | artículo |
| Fecha de publicación: | 1986 |
| 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:10272/18496 |
| Acesso em linha: | http://hdl.handle.net/10272/18496 |
| Access Level: | acceso abierto |
| Palavra-chave: | Transpressive thrust Normal faults Extensional structure Gibraltar Arc |
| Resumo: | Constitutive units of Alboran and Sudiberic Domains near Gibraltar Arc are specified. The boundary between both domains results from a crustal scale westward transpressive thrust and superimposed Iow angle normal faults later developed. Thus most of the tectonic contacts presently observed are extensional in character |
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