RT Journal Article
T1 Fluidos asociados a la formación de epidota + (clorita + cuarzo) en las pegmatitas del plutón de La Cabrera (Sistema Central Español)
T1 Fluids associated to epidote + (chlorite + quartz) in pegmatites from La Cabrera pluton (Spanish Central System)
A1 Lozano Fernández, R. P.
A1 Bachiller, N.
A1 Casquet Martín, César
AB Fluids related to the epidote+chlorite+quartz and calcite (Flaumont/te) alterations present in the cores of pegmatites from La Cabrera pluton have been determined. Two types of fluids are involved: a) Alow salinity (0.4-4.5 wt% NaCI equiv.) NaCI-H20 fluid is the responsable for the first type ofalteration. Temperature was probably dose to 300°C. b) A moderate to high salinity (15.3-24.5 wt% Nad equiv.) heterogeneous (liquid + gas) CaCi2-NaCt-H20 fluid was involved in the second alteration under conditions of PffM probably very dose to hydrostatic. These alterations probably took place as discrete hydrothermal events of different ages
PB Sociedad Geológica de España
YR 1996
FD 1996
LK http://hdl.handle.net/10272/11086
UL http://hdl.handle.net/10272/11086
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026