Sedimentología de los materiales terciarios de la cubeta intramontañosa de El Rásilio.(Sierra de Cameros, La Rioja)

Sédimentology of the Tertiary deposits of the El Rasillo intramountainous basin (Cameros Range, La Rioja)

dc.contributor.author	Molinero Huguet, J.
dc.contributor.author	Colombo Piñol, Ferrán
dc.date.accessioned	2017-03-09T12:09:06Z
dc.date.available	2017-03-09T12:09:06Z
dc.date.issued	1995
dc.identifier.uri	http://hdl.handle.net/10272/13438
dc.description.abstract	El Rasillo intramountainous basin, with 300 m of minimun thickness of Oligocene-Miocene alluvial sediments, is located in Cameros Mesozoic Unit and next to La Demandai Paleozoic Unit. The sedimentological analysis of the sedimentary rocks allows us to make out four alluvial systems, coming from different source areas during the filling of this basin. No features of synsedimentary tectonics have been found, suggesting that the main allocyclic control, of these alluvial systems was the climate	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	Cameros Range	en_US
dc.subject.other	Intramountainous basin	en_US
dc.subject.other	Oligocene-Miocene	en_US
dc.subject.other	Alluvial fan	en_US
dc.title	Sedimentología de los materiales terciarios de la cubeta intramontañosa de El Rásilio.(Sierra de Cameros, La Rioja)	en_US
dc.title	Sédimentology of the Tertiary deposits of the El Rasillo intramountainous basin (Cameros Range, La Rioja)	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

Sédimentology of the Tertiary deposits of the El Rasillo intramountainous basin (Cameros Range, La Rioja)

dc.contributor.author	Molinero Huguet, J.
dc.contributor.author	Colombo Piñol, Ferrán
dc.date.accessioned	2017-03-09T12:09:06Z
dc.date.available	2017-03-09T12:09:06Z
dc.date.issued	1995
dc.identifier.uri	http://hdl.handle.net/10272/13438
dc.description.abstract	El Rasillo intramountainous basin, with 300 m of minimun thickness of Oligocene-Miocene alluvial sediments, is located in Cameros Mesozoic Unit and next to La Demandai Paleozoic Unit. The sedimentological analysis of the sedimentary rocks allows us to make out four alluvial systems, coming from different source areas during the filling of this basin. No features of synsedimentary tectonics have been found, suggesting that the main allocyclic control, of these alluvial systems was the climate	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	Cameros Range	en_US
dc.subject.other	Intramountainous basin	en_US
dc.subject.other	Oligocene-Miocene	en_US
dc.subject.other	Alluvial fan	en_US
dc.title	Sedimentología de los materiales terciarios de la cubeta intramontañosa de El Rásilio.(Sierra de Cameros, La Rioja)	en_US
dc.title	Sédimentology of the Tertiary deposits of the El Rasillo intramountainous basin (Cameros Range, La Rioja)	eng
dc.type	info:eu-repo/semantics/article	en_US
dc.rights.accessRights	info:eu-repo/semantics/openAccess	en_US

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