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Quaternary phases of chemical sedimentation in los Covachos cave (Almadén de la Plata, Seville)

dc.contributor.authorRodríguez Vidal, Joaquín 
dc.contributor.authorÁlvarez García, G.
dc.contributor.authorAlcaraz, J. M.
dc.contributor.authorMartínez Aguirre, Arancha
dc.contributor.authorCáceres Puro, Luis Miguel 
dc.contributor.authorCantano Martín, Mercedes 
dc.contributor.authorCaro Gómez, J. A.
dc.description.abstractThe geological and geomorphological studies in Los Covachos cave reveal a wide collection of speleothems and a thick archaeological stratigraphies. Both isotopie dating of speleothems C^ThP^U) and charcoal layers C4C), in chemical and terrigenous sediments, show a Quaternary sequence of palaeoenvironmental evolution related with an alternating phases of biostatic and rhexistatic genesis. The first ones are partially situated in a warm and wet isotopie stages (7, 5, 3, and 1) and the others in a wider warm and dry stages (6, 4 and 2)en_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherIsotopie datingen_US
dc.subject.otherSierra Morenaen_US
dc.titleEpisodios cuaternarios de sedimentación química en la cueva de Los Covachos (Almadén de la Plata, Sevilla)en_US
dc.titleQuaternary phases of chemical sedimentation in los Covachos cave (Almadén de la Plata, Seville)eng

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