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Rock mass classification of slate sequences in The Truchas Syncline

dc.contributor.authorRodríguez Sastre, M. A.
dc.date.accessioned2014-07-16T09:30:08Z
dc.date.available2014-07-16T09:30:08Z
dc.date.issued2006
dc.identifier.urihttp://hdl.handle.net/10272/8560
dc.description.abstractRock mass characterization and classification are significant in geological investigations involving engineering works and in the field of applied geology. Discontinuities characterization and rock properties determination are essential within the intended engineering work type. An outcrop of the metamorphic rocks from Casio Formation at The Truchas Syncline has been the target of this investigation. The most widely used rock mass classification systems are the Rock Mass Quality Index (Q system) and the Geomechanics Classification (RMR) and more recently the SRC system and those were applied in this site of investigation. Fair rock with a III RMR class has been described for this outcrop under investigation while Q rock mass classification is set between very poor and poor in that site. In addition the SRC classification provide a class V rock massen_US
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherSlatesen_US
dc.subject.otherDiscontinuitiesen_US
dc.subject.otherCasaio Formationen_US
dc.subject.otherRock mass classificationen_US
dc.titleClasificación geomecánica de macizos pizarrosos en el sinclinal de Truchasen_US
dc.titleRock mass classification of slate sequences in The Truchas Synclineeng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess


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