Mega-debris flows en el tránsito Devónico-Carbonífero de la Faja Pirítica Ibérica

dc.contributor.authorMoreno Garrido, María Carmen
dc.contributor.authorSierra del Pino, Sonia
dc.contributor.authorSáez Ramos, Reinaldo
dc.date.accessioned2017-06-06T11:00:41Z
dc.date.available2017-06-06T11:00:41Z
dc.date.issued1994
dc.description.abstractDetrital platform sedimentation during the Devonian times took place in the homogeneous basin of the Iberian Pyrite Belt. This shallow basin changed to a mosaic of horsts and grabens just in the Devonian-Carboniferous boundary. Thick mattrix supported conglomerates (mega-debris flow) appear related with this dynamic. They suggest convulsive seismic events related to the Breton phase of the Hercynian orogenyen_US
dc.identifier.urihttp://hdl.handle.net/10272/13792
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherDevonianen_US
dc.subject.otherMega-debris flowen_US
dc.subject.otherIberian Pyrite Belten_US
dc.titleMega-debris flows en el tránsito Devónico-Carbonífero de la Faja Pirítica Ibéricaen_US
dc.titleMega-debris flows in the Devonian-Carboniferous boundary of the Iberian Pyrite Belteng
dc.typejournal articleen_US
dspace.entity.typePublication
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relation.isAuthorOfPublication838bf493-d713-49fc-8ecc-8f9bb3aa81e6
relation.isAuthorOfPublication3b6223ac-76bd-4294-a809-3c0f36c999ce
relation.isAuthorOfPublication.latestForDiscovery00d321ab-feb5-412c-ab90-de35f0372e86

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