Estructuras extensionales en los materiales Aipujárrides al E de Málaga (Sierra Tejeda, Cordilleras Béticas)

The main deformation in the Tejeda and Canillas de Albaida Units is produced during a heterogeneous simple shearing regime that generates a planar-linear fabric. This simple shear has a topto-the-westsouhwest sense of movement. Later overturned north-vergent folds and brittle deformations associated...

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Detalles Bibliográficos
Autores: Fernández Fernández, Estefanía, Campos, J., González Lodeiro, Francisco
Tipo de recurso: artículo
Fecha de publicación:1992
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:10272/16337
Acceso en línea:http://hdl.handle.net/10272/16337
Access Level:acceso abierto
Palabra clave:Betic Cordilleras
Extensional tectonic
Detachment
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spelling Estructuras extensionales en los materiales Aipujárrides al E de Málaga (Sierra Tejeda, Cordilleras Béticas) Extensional structures in the Alpujarride materials of the East of Malaga (Sierra Tejeda, Betic Cordilleras) Fernández Fernández, Estefanía Campos, J. González Lodeiro, Francisco Betic Cordilleras Extensional tectonic Detachment The main deformation in the Tejeda and Canillas de Albaida Units is produced during a heterogeneous simple shearing regime that generates a planar-linear fabric. This simple shear has a topto-the-westsouhwest sense of movement. Later overturned north-vergent folds and brittle deformations associated to normal faults with a top-to-the-westsouthwest sense of movement affect the previous structures. The normal fault (Alcaucm Fault) that separates the Sierra Tejeda Unit (footwall) from the Canillas and Sayalonga Units (hanging wall) is a detachment. Normal faults that separate the different units of the hanging wall joint the detachment and they do not penetrate into the footwall Sociedad Geológica de España http://hdl.handle.net/10272/16337
title Estructuras extensionales en los materiales Aipujárrides al E de Málaga (Sierra Tejeda, Cordilleras Béticas)
spellingShingle Estructuras extensionales en los materiales Aipujárrides al E de Málaga (Sierra Tejeda, Cordilleras Béticas)
Fernández Fernández, Estefanía
Betic Cordilleras
Extensional tectonic
Detachment
title_short Estructuras extensionales en los materiales Aipujárrides al E de Málaga (Sierra Tejeda, Cordilleras Béticas)
title_full Estructuras extensionales en los materiales Aipujárrides al E de Málaga (Sierra Tejeda, Cordilleras Béticas)
title_fullStr Estructuras extensionales en los materiales Aipujárrides al E de Málaga (Sierra Tejeda, Cordilleras Béticas)
title_full_unstemmed Estructuras extensionales en los materiales Aipujárrides al E de Málaga (Sierra Tejeda, Cordilleras Béticas)
title_sort Estructuras extensionales en los materiales Aipujárrides al E de Málaga (Sierra Tejeda, Cordilleras Béticas)
author Fernández Fernández, Estefanía
author_facet Fernández Fernández, Estefanía
Campos, J.
González Lodeiro, Francisco
author_role author
author2 Campos, J.
González Lodeiro, Francisco
author2_role author
author
topic Betic Cordilleras
Extensional tectonic
Detachment
topic_facet Betic Cordilleras
Extensional tectonic
Detachment
description The main deformation in the Tejeda and Canillas de Albaida Units is produced during a heterogeneous simple shearing regime that generates a planar-linear fabric. This simple shear has a topto-the-westsouhwest sense of movement. Later overturned north-vergent folds and brittle deformations associated to normal faults with a top-to-the-westsouthwest sense of movement affect the previous structures. The normal fault (Alcaucm Fault) that separates the Sierra Tejeda Unit (footwall) from the Canillas and Sayalonga Units (hanging wall) is a detachment. Normal faults that separate the different units of the hanging wall joint the detachment and they do not penetrate into the footwall
publishDate 1992
format article
url http://hdl.handle.net/10272/16337
language spa
eu_rights_str_mv openAccess
publisher Sociedad Geológica de España
institution Universidad de Huelva (UHU)
collection Arias Montano. Repositorio Institucional de la Universidad de Huelva
reponame_str Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname_str Universidad de Huelva (UHU)
_version_ 1878437012307968000
publishDateSort 1992
author_browse Campos, J.
Fernández Fernández, Estefanía
González Lodeiro, Francisco
publisherStr Sociedad Geológica de España
score 6,924472