Aproximación a la hidrodinámica de los sistemas hidrotermales «liquido-dominantes» asociados a yacimientos de Au-Ag. Aplicación teórica al sector Almagrera-Herrerías (Almería)
DOI:
https://doi.org/10.3989/egeol.94503-4317Keywords:
Epithermal, numerical model, convection, hydrothermalAbstract
Epithermal mineralization of Almagrera-Herrerías area is related to a hydrothermal system wich is formed by superficial convective cells fed by meteoric marine and magmatic waters. Mathematical simulation of a theoretical hydrothermal convective system, shows a coincidence between ore deposits and mass discharge and accumulation areas, predicted by a numerical model. Previous conclusions, together with the existence of a hydrothermal system still active, explains the interest to localize discharge areas of the hydrogeological system, in order to Know the mineral deposits genesis, and to search for new mineralizations.
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