
handle: 10272/11086 , 20.500.14352/56936
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
Ca-alterations, 552.3(234.1), Petrología, Spanish Central System., Pegmatites, Spanish Central System, Fluid inclusions
Ca-alterations, 552.3(234.1), Petrología, Spanish Central System., Pegmatites, Spanish Central System, Fluid inclusions
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