RT Journal Article
T1 Travertinos ligados a fallas: ejemplos del desierto de Tabernas (Almería, Cordillera Bética)
T1 Travertines linked to faults. Examples from the Tabernas desert (Almeria, Betic Cordillera)
A1 Sanz de Galdeano, Carlos
A1 Galindo Zaldívar, Jesús
A1 Morales, Salvador
A1 López Chicano, Manuel
A1 Azañón, José Miguel
A1 Martín Rosales, Wenceslao
AB In the Tabernas desert there are several sectors with Quaternary travertines not formed in the proximitiesof carbonatic rocks, but originated by the rise of deep mineralized water along faults. These travertineshave Fe mineralization in its older levels. The mineralization present similitude with that formed in theregion during the late Miocene, then connected with the volcanism
YR 2008
FD 2008
LK http://hdl.handle.net/10272/8203
UL http://hdl.handle.net/10272/8203
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 29 may 2026