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Polyphase karstification processes in Crema Marfil quarries (Pinoso, Alicante). Application to exploitation of dimension stones

dc.contributor.authorCañaveras, J.C.
dc.contributor.authorGarcía del Cura, María Angeles
dc.contributor.authorSánchez Moral, S.
dc.contributor.authorMuñoz Cervera, M. C.
dc.contributor.authorOrdóñez, Salvador
dc.description.abstractComplex speleothem networks have been recognised in the quarries of the commercial marble Crema Marfil (Paleogene limestones, Monte Coto Pinoso, Alicante). The characterisation of these speleothems (mineralogy, petrography, stable isotopes) has enable us to discriminate different phases of speleothem formation in terms of paleotemperature or structural control. U/Th dates of some of these phases are 178,7± 15,6 Ka, 34,4+1,7 Ka y 33,7±3,4 Ka. A seismo-tectonic event has been recorded and dated (33-34Ka) by the study of speleothems. The recognition and characterisation of speleothem networks can be considered as a useful tool in the design of exploitation strategies of dimension stonesen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherCrema Marfilen_US
dc.subject.otherStable isotopesen_US
dc.titleProcesos de karstíficación polifásica en las canteras de Crema Marfil (Pinoso, Alicante). Aplicación a la explotación de rocas ornamentalesen_US
dc.titlePolyphase karstification processes in Crema Marfil quarries (Pinoso, Alicante). Application to exploitation of dimension stoneseg

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