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dc.contributor.authorPereira Gómez, María Dolores es_ES
dc.contributor.authorYenes Ortega, Mariano es_ES
dc.contributor.authorBlanco Sánchez, José Antonioes_ES
dc.contributor.authorPeinado Moreno, María Mercedeses_ES
dc.date.accessioned2009-03-11es_ES
dc.date.accessioned2009-10-07T11:41:48Z
dc.date.available2009-10-07T11:41:48Z
dc.date.issued2007es_ES
dc.identifier.citationPEREIRA, D., YENES, M.,BLANCO,J.A., PEINADO, M. Characterization of serpentinites to define their appropriate use as dimension stone. En R. Prikryl and B. J. Smith (Eds.), "Building stone decay: from diagnosis to conservation (pp. 55-62). London: Geological Society.es_ES
dc.identifier.urihttp://hdl.handle.net/10366/19418es_ES
dc.identifier.urihttp://hdl.handle.net/10366/19418
dc.description.abstractAbstract: Many questions arise when considering the appropriate use of building stones such as serpentinites. The commercial names of these rocks, collectively grouped as Green marbles ,have no correspondence to their actual mineralogy, geochemistry and/or physical characteristics. Serpentinite being the hydrated product of an ultramafic parent rock and not a metamorphicproduct of limestone as implied by the term marble . However, the serpentinites most widely used for ornamental purposes come from India (e.g. Rajasthan Green, Emerald Green) and in these the original mineralogy has been almost completely converted into carbonates. By contrast,serpentinites from elsewhere (e.g. Vermont Verde Antique from the USA and Verde Pirineos from Spain) do preserve some of their original mineralogy. The different physical and chemicalbehaviour of carbonates and serpentine minerals can result in significantly different behaviour of commercial building stones. Thus, carbonates are resistant to weathering but suffer fromacidic cleaning agents in interior use; whereas serpentinites, with a high content of talc, used on external faces undergo an increase in volume and a consequent rapid degradation. Accurate and precise characterization of serpentinites, including information on their mineralogyand geochemistry (including major, trace and volatile elements together with oxygenisotopes), in conjunction with their physical properties, would enable architects to select the appropriate interior or exterior use of these handsome building stones.es_ES
dc.format.extent8 p.es_ES
dc.format.mimetypeapplication/pdfes_ES
dc.languageIngléses_ES
dc.language.isoenges_ES
dc.publisherGeological Society of London (Londres, Gran Bretaña)es_ES
dc.relation.requiresAdobe Acrobates_ES
dc.rightsAttribution-NonCommercial-NoDerivs 3.0 Unported
dc.rights.urihttps://creativecommons.org/licenses/by-nc-nd/3.0/
dc.subjectSerpentinitases_ES
dc.subjectGeoquímicaes_ES
dc.subjectPiedra de construcciónes_ES
dc.subjectConservación y restauraciónes_ES
dc.subjectSerpentiniteses_ES
dc.subjectGeochemistryes_ES
dc.subjectBuilding stonees_ES
dc.titleCharacterization of serpentinites to define their appropriate use as dimension stonees_ES
dc.typeinfo:eu-repo/semantics/bookPartes_ES
dc.typeinfo:eu-repo/semantics/bookPartes_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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