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handle: 10261/29437 , 10272/8203
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.
Este estudio ha sido financiado por los proyectos CICYT CSD2006-00041, CGL2007- 60535, Junta de Andalucía P06RNM- 01521, RNM- y AECI A.012371.07 y 83/ 2007 de M.M.A.
4 páginas, 5 figuras.-- Trabajo presentado en la 45ª Sesión Científica, Bilbao, 2008.
Peer reviewed
Quaternary, Travertines, Faults, Fe mineralization
Quaternary, Travertines, Faults, Fe mineralization
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