Corte balanceado de la Sierra Cantabria (cabalgamiento de la Cuenca Vasco-Cantábrica sobre la Cuenca del Ebro)

Balanced cross-section of the Sierra Cantabria (Basque-Cantabrian basin thrust on the Ebro basin)

dc.contributor.author	Martínez Torres, Luis M.
dc.date.accessioned	2017-08-09T11:27:05Z
dc.date.available	2017-08-09T11:27:05Z
dc.date.issued	1993
dc.identifier.uri	http://hdl.handle.net/10272/14024
dc.description.abstract	On the transversal of Puerto de Herrera (Alava), the southern limit of the Basque-Cantabrian basin thrusts on the Ebro basin in favour of two thrusting sequences. The minimum shortening measured exceeds 35% with a 3.25 kilometers stacking of the series at the front. Besides, a transport of the materials of ovrer 15 kilometers can be deduced. The thrustings were generated from the tectonic inversion of the normal faults which conditioned the Upper Cretacious deposit and, perhaps, an early diapirism	es_ES
dc.language.iso	spa	es_ES
dc.publisher	Sociedad Geológica de España	es_ES
dc.rights	Atribución-NoComercial-SinDerivadas 3.0 España	*
dc.rights.uri	http://creativecommons.org/licenses/by-nc-nd/3.0/es/	*
dc.subject.other	Balanced cross-section	es_ES
dc.subject.other	Tectonic inversion	es_ES
dc.subject.other	Diapirism	es_ES
dc.subject.other	Alpine orogeny	es_ES
dc.subject.other	Ebro basin	es_ES
dc.subject.other	Basque Cantabrian basin	es_ES
dc.title	Corte balanceado de la Sierra Cantabria (cabalgamiento de la Cuenca Vasco-Cantábrica sobre la Cuenca del Ebro)	es_ES
dc.title	Balanced cross-section of the Sierra Cantabria (Basque-Cantabrian basin thrust on the Ebro basin)	eng
dc.type	info:eu-repo/semantics/article	es_ES
dc.rights.accessRights	info:eu-repo/semantics/openAccess	es_ES

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

Balanced cross-section of the Sierra Cantabria (Basque-Cantabrian basin thrust on the Ebro basin)

dc.contributor.author	Martínez Torres, Luis M.
dc.date.accessioned	2017-08-09T11:27:05Z
dc.date.available	2017-08-09T11:27:05Z
dc.date.issued	1993
dc.identifier.uri	http://hdl.handle.net/10272/14024
dc.description.abstract	On the transversal of Puerto de Herrera (Alava), the southern limit of the Basque-Cantabrian basin thrusts on the Ebro basin in favour of two thrusting sequences. The minimum shortening measured exceeds 35% with a 3.25 kilometers stacking of the series at the front. Besides, a transport of the materials of ovrer 15 kilometers can be deduced. The thrustings were generated from the tectonic inversion of the normal faults which conditioned the Upper Cretacious deposit and, perhaps, an early diapirism	es_ES
dc.language.iso	spa	es_ES
dc.publisher	Sociedad Geológica de España	es_ES
dc.rights	Atribución-NoComercial-SinDerivadas 3.0 España	*
dc.rights.uri	http://creativecommons.org/licenses/by-nc-nd/3.0/es/	*
dc.subject.other	Balanced cross-section	es_ES
dc.subject.other	Tectonic inversion	es_ES
dc.subject.other	Diapirism	es_ES
dc.subject.other	Alpine orogeny	es_ES
dc.subject.other	Ebro basin	es_ES
dc.subject.other	Basque Cantabrian basin	es_ES
dc.title	Corte balanceado de la Sierra Cantabria (cabalgamiento de la Cuenca Vasco-Cantábrica sobre la Cuenca del Ebro)	es_ES
dc.title	Balanced cross-section of the Sierra Cantabria (Basque-Cantabrian basin thrust on the Ebro basin)	eng
dc.type	info:eu-repo/semantics/article	es_ES
dc.rights.accessRights	info:eu-repo/semantics/openAccess	es_ES

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