Resistencia al rebote en materiales de la Formación Casaio (Ordovícico del NO de España)

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dc.contributor.authorRodríguez Sastre, M. A.
dc.contributor.authorGutiérrez Claverol, M.
dc.contributor.authorTorres Alonso, M.
dc.contributor.authorRodríguez Bouzo, M.
dc.date.accessioned2014-10-23T10:08:49Z
dc.date.available2014-10-23T10:08:49Z
dc.date.issued2004
dc.description.abstractSeveral types of Ordovician Rocks (Casaio Formation in Truchas Synclinal) have been tested with the Schmidt hammer, model L. The compressive strength of these rocks has been estimated by the rebound values "in situ" and "in rock blocks" as very different from low to very high in order to its weathering and cleavage positionen_US
dc.identifier.urihttp://hdl.handle.net/10272/8958
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.otherRebound strengthen_US
dc.subject.otherSchmidt hammeren_US
dc.subject.otherCasaio Formationen_US
dc.subject.otherOrdovicianen_US
dc.subject.otherNW Spainen_US
dc.titleResistencia al rebote en materiales de la Formación Casaio (Ordovícico del NO de España)en_US
dc.titleRebound strength on Casaio Formation rocks (Ordovician from thé AIW of Spain)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 36, (2004)