Neoformación de sales en la piedra monumental de la Ciudad de Zamora

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dc.contributor.authorAñorbe Urmeneta, M.
dc.contributor.authorSáinz de Cueto, F. J.
dc.contributor.authorMartín Pozas, J. M.
dc.contributor.authorDíez Torres, J. A.
dc.date.accessioned2016-11-10T12:51:32Z
dc.date.available2016-11-10T12:51:32Z
dc.date.issued1996
dc.description.abstractIn this paper special focus is placed on the neoformation of salts (gypsum, halite, calcite, dolomite and calcic oxalates) and stone deterioration mechanisms concerning the main historical monuments of Zamora (Spain). Several measuring techniques and assessment methods are been developed. Some explanatory attempts about the neoconstituent compounds causality are proposed.en_US
dc.identifier.urihttp://hdl.handle.net/10272/12821
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.otherOrnamental stoneen_US
dc.subject.otherNeoformationen_US
dc.subject.otherSaltsen_US
dc.subject.otherZamoraen_US
dc.subject.otherSpainen_US
dc.titleNeoformación de sales en la piedra monumental de la Ciudad de Zamoraen_US
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 20-5, (1996)