Distribución geoquímica de elementos traza en los sulfuros pirita y cinabrio y en las intercalaciones pizarrosas de la capa de San Nicolás. Yacimiento de Almaden (Ciudad Real)
DOI:
https://doi.org/10.3989/egeol.88443-4536Keywords:
Pyrite, Cínnabar, Geochemistry, Trace elements, AlmadénAbstract
The «Cuarcita del Criadero» of the Almadén ore Deposit is formed by two quartzitic zones, one upper and the other lower, separated by the denominated intermediate shales. The Upperr Quartzitic Zone comprises of the banging to the foot wall: the mineralized Iayer of «San Nicolás», the mineralized layer of «San Francisco» and the Intermediate Quartzites whereas the Lower Quartzitic Zone contains the mineralized layer of «San Pedro». In the present paper, we investigate, by means of plasma emission spectrometry by inductive coupling the distribution of certain trace elements, thirteen in pyrites, twelve in cinnabars and seventeen in the shaly strata of the mineralized layer of «San Nicolás», in order to establish the geochemical character of the pyrite, cinnabar and of the shaly strata just as the origin of the two sulphides.
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