Variaciones laterales del "Nivel de Fuentes", Precámbrico-Cámbrico de la Zona Centro-Ibérica

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dc.contributor.authorSantamaría Casanovas, J.
dc.contributor.authorRemacha Grau, Eduard
dc.date.accessioned2017-08-07T10:41:00Z
dc.date.available2017-08-07T10:41:00Z
dc.date.issued1994
dc.description.abstractThe "Nivel de Fuentes", in the Valdelacasa Allogroup (Precambrian-Cambrian), can be divided in five subunits. Each one of them is build-up by a basal megabreccia overlaid by a fine-grained turbidite wedge that tends to pinch-out toward the central region of the Valdelacasa anticline. The isochron character ofthe "Nivel de Fuentes" is rejected because really it is multieventes_ES
dc.identifier.urihttp://hdl.handle.net/10272/14015
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accesses_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherMegabrecciaes_ES
dc.subject.otherNivel de Fuenteses_ES
dc.subject.otherSeismic-eventes_ES
dc.subject.otherPrecambrian-Cambrianes_ES
dc.subject.otherCentral-lberian Zonees_ES
dc.titleVariaciones laterales del "Nivel de Fuentes", Precámbrico-Cámbrico de la Zona Centro-Ibéricaes_ES
dc.titleLateral changes in the "Nivel de Fuentes", Precambrían-Cambrían ofthe Central-Iberian Zone.eng
dc.typejournal articlees_ES
dspace.entity.typePublication

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Geogaceta -- Nº 15, (1993)