@article{10272/14056,
year = {1993},
url = {http://hdl.handle.net/10272/14056},
abstract = {Late Zn-rich assemblages have been found in several lithilogies of the Bédar-Macael unit and upper part of the Calar-Alto unit (Nevado-Filabride Complex). The nowadays brittle contacts between the nevado-filábride and alpujárride units are low-angle normal faults of an extensional system Middle Miocene in age. In metabasite rocks of the Bédar-Macael unit, Zn-rich staurolite (ZnO<13 wt%) partially transformed to gahnite-haematite+quartz assemblage has been found},
publisher = {Sociedad Geológica de España},
keywords = {Zn-rich staurolite},
keywords = {Hydrothermal fluids},
keywords = {Extensional shear zones},
keywords = {Brittle-ductile transition},
keywords = {Betics},
title = {Presencia de mineralogías ricas en Zn como evidencias de la actividad hidrotermal enzonas de cizalla extensionales (Complejo Nevado-Filábride, Béticas)},
title = {Occurrence of Zn-rich assemblages controled   by hydrothermal activity in extensional shear zones (Nevado-Filábride Complex, Betics)},
author = {Soto, Juan I. and Muñoz, Mercedes},
}