Caracterización sedimentológica de un nivel guía y su posible origen sísmico, Corredor del Almanzora (Almería)

dc.contributor.author	Sola, Fernando
dc.date.accessioned	2013-11-21T11:54:58Z
dc.date.available	2013-11-21T11:54:58Z
dc.date.issued	2010
dc.description.abstract	A conglomeratic level intercalated in a turbiditic sequence in the Almanzora corridor (Betic Cordillera) has been mapped. This level is 3 to 15 m thick, with clasts bigger than 3 m diameter. It can be continued along 6 km, which makes it being a good key bed in the study area. The level origin has been interpreted as a collapse deposit from the southern margin of the basin, probably due to a seismic event	en_US
dc.identifier.uri	http://hdl.handle.net/10272/7460
dc.language.iso	spa	en_US
dc.publisher	Universidad de Huelva	en_US
dc.rights	Atribución-NoComercial-SinDerivadas 3.0 España
dc.rights.accessRights	open access
dc.rights.uri	http://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.other	Key bed	en_US
dc.subject.other	Seismite	en_US
dc.subject.other	Gordo Megabed	en_US
dc.subject.other	Almanzora Corridor	en_US
dc.title	Caracterización sedimentológica de un nivel guía y su posible origen sísmico, Corredor del Almanzora (Almería)	en_US
dc.title	Sedimentologic characterization of a key bed: a possible seismic origin (Almanzora Corridor, Almería)	eng
dc.type	journal article	en_US
dspace.entity.type	Publication

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