Estructura y cinemática de la falla de Alpeñés (Cordillera Ibérica)

Structure and Kinematics of the Alpeñés fault (Iberian Chain)

dc.contributor.author	Tena, S.
dc.contributor.author	Casas Sainz, Antonio
dc.date.accessioned	2016-08-25T11:11:47Z
dc.date.available	2016-08-25T11:11:47Z
dc.date.issued	1996
dc.identifier.uri	http://hdl.handle.net/10272/12561
dc.description.abstract	The Alpenes anticline is a detachment fold of the Jurassic-Cretaceous cover, whose location and geometry is controlled by the Alpenes NNE-SSW-trending basement fault. This fault constituted the southwestern margin of the Aliaga basin (Iberian Chain) during the Cretaceous, with a normal movement slipping northwards and was re-activated during the Tertiary compression as a right-lateral strike-slipreverse fault The cumulative heave of the Alpehes fault in the detached mesozoic cover is about 400 m, the western block being uplifted with respect to the eastern block during the mesozoic extension and tertiary inversion.	en_US
dc.language.iso	spa	en_US
dc.publisher	Sociedad Geológica de España	en_US
dc.rights	Atribución-NoComercial-SinDerivadas 3.0 España	*
dc.rights.uri	http://creativecommons.org/licenses/by-nc-nd/3.0/es/	*
dc.subject.other	Detachment fold	en_US
dc.subject.other	Basement fault	en_US
dc.subject.other	Alpenes fault	en_US
dc.subject.other	Iberian Chain	en_US
dc.title	Estructura y cinemática de la falla de Alpeñés (Cordillera Ibérica)	en_US
dc.title	Structure and Kinematics of the Alpeñés fault (Iberian Chain)	eng
dc.type	info:eu-repo/semantics/article	en_US
dc.rights.accessRights	info:eu-repo/semantics/openAccess	en_US

Except where otherwise noted, this item's license is described as Atribución-NoComercial-SinDerivadas 3.0 España

Structure and Kinematics of the Alpeñés fault (Iberian Chain)

dc.contributor.author	Tena, S.
dc.contributor.author	Casas Sainz, Antonio
dc.date.accessioned	2016-08-25T11:11:47Z
dc.date.available	2016-08-25T11:11:47Z
dc.date.issued	1996
dc.identifier.uri	http://hdl.handle.net/10272/12561
dc.description.abstract	The Alpenes anticline is a detachment fold of the Jurassic-Cretaceous cover, whose location and geometry is controlled by the Alpenes NNE-SSW-trending basement fault. This fault constituted the southwestern margin of the Aliaga basin (Iberian Chain) during the Cretaceous, with a normal movement slipping northwards and was re-activated during the Tertiary compression as a right-lateral strike-slipreverse fault The cumulative heave of the Alpehes fault in the detached mesozoic cover is about 400 m, the western block being uplifted with respect to the eastern block during the mesozoic extension and tertiary inversion.	en_US
dc.language.iso	spa	en_US
dc.publisher	Sociedad Geológica de España	en_US
dc.rights	Atribución-NoComercial-SinDerivadas 3.0 España	*
dc.rights.uri	http://creativecommons.org/licenses/by-nc-nd/3.0/es/	*
dc.subject.other	Detachment fold	en_US
dc.subject.other	Basement fault	en_US
dc.subject.other	Alpenes fault	en_US
dc.subject.other	Iberian Chain	en_US
dc.title	Estructura y cinemática de la falla de Alpeñés (Cordillera Ibérica)	en_US
dc.title	Structure and Kinematics of the Alpeñés fault (Iberian Chain)	eng
dc.type	info:eu-repo/semantics/article	en_US
dc.rights.accessRights	info:eu-repo/semantics/openAccess	en_US

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