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Travertinos ligados a fallas: ejemplos del desierto de Tabernas (Almería, Cordillera Bética)

Authors: Sanz de Galdeano, Carlos; Galindo Zaldívar, Jesús; Morales, Salvador; López Chicano, Manuel; Azañón, José Miguel; Martín Rosales, Wenceslao;

Travertinos ligados a fallas: ejemplos del desierto de Tabernas (Almería, Cordillera Bética)

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.

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

Country
Spain
Related Organizations
Keywords

Quaternary, Travertines, Faults, Fe mineralization

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popularity
This indicator reflects the "current" impact/attention (the "hype") of an article in the research community at large, based on the underlying citation network.
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influence
This indicator reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
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impulse
This indicator reflects the initial momentum of an article directly after its publication, based on the underlying citation network.
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