Estudio preliminar sobre la tectónica sinsedimentaria del Cretácico inferior en el borde septentrional de la Cubeta de Aliaga (Cordillera Ibérica)

Preliminary study of the Lower Cretaceous synsedimentary tectonics in the northern border of Aliaga sub-basin (Iberian Chain)

dc.contributor.author	Liesa, Carlos L.
dc.contributor.author	Soria, Ana Rosa
dc.contributor.author	Meléndez Hevia, Alfonso
dc.date.accessioned	2017-01-26T12:57:04Z
dc.date.available	2017-01-26T12:57:04Z
dc.date.issued	1996
dc.identifier.uri	http://hdl.handle.net/10272/13201
dc.description.abstract	The Aliaga sub-basin was developed during the Early Cretaceous in an extensional context. Structures near the northern border of this sub-basin (normal faults, syntectonic unconformities and facies and thickness changes in the basin infill) are related to this extensional tectonics. The graben and semigraben system determines the syntectonic infill thickness. In the footwall of the main faults the pre-rift sequence is eroded	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	Synsedimentary tectonic	en_US
dc.subject.other	Lower Cretaceous	en_US
dc.subject.other	Aliaga sub-basin	en_US
dc.title	Estudio preliminar sobre la tectónica sinsedimentaria del Cretácico inferior en el borde septentrional de la Cubeta de Aliaga (Cordillera Ibérica)	en_US
dc.title	Preliminary study of the Lower Cretaceous synsedimentary tectonics in the northern border of Aliaga sub-basin (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

Preliminary study of the Lower Cretaceous synsedimentary tectonics in the northern border of Aliaga sub-basin (Iberian Chain)

dc.contributor.author	Liesa, Carlos L.
dc.contributor.author	Soria, Ana Rosa
dc.contributor.author	Meléndez Hevia, Alfonso
dc.date.accessioned	2017-01-26T12:57:04Z
dc.date.available	2017-01-26T12:57:04Z
dc.date.issued	1996
dc.identifier.uri	http://hdl.handle.net/10272/13201
dc.description.abstract	The Aliaga sub-basin was developed during the Early Cretaceous in an extensional context. Structures near the northern border of this sub-basin (normal faults, syntectonic unconformities and facies and thickness changes in the basin infill) are related to this extensional tectonics. The graben and semigraben system determines the syntectonic infill thickness. In the footwall of the main faults the pre-rift sequence is eroded	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	Synsedimentary tectonic	en_US
dc.subject.other	Lower Cretaceous	en_US
dc.subject.other	Aliaga sub-basin	en_US
dc.title	Estudio preliminar sobre la tectónica sinsedimentaria del Cretácico inferior en el borde septentrional de la Cubeta de Aliaga (Cordillera Ibérica)	en_US
dc.title	Preliminary study of the Lower Cretaceous synsedimentary tectonics in the northern border of Aliaga sub-basin (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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