Travertinos ligados a fallas: ejemplos del desierto de Tabernas (Almería, Cordillera Bética)
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Abstract
In the Tabernas desert there are several sectors with Quaternary travertines not formed in the proximities
of carbonatic rocks, but originated by the rise of deep mineralized water along faults. These travertines
have Fe mineralization in its older levels. The mineralization present similitude with that formed in the
region during the late Miocene, then connected with the volcanism
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