RT Journal Article
T1 Fluidos asociados a la formación de epidota + (clorita + cuarzo) enlas pegmatitas del plutón de La Cabrera (Sistema Central Español)
A1 Lozano Fernández, Rafael Pablo
A1 Bachiller Jareño, Nuria
A1 Casquet, César
AB Fluids related to the epidote+chlorite+quartz and calcite (+laumontite) alterations present in thecores of pegmatites from La Cabrera pluton have been determined. Two types of fluids are in volved: a)A low salinity (0.4-4.5 wt% NaCl equiv.) NaCl-H20 fluid is the responsable for the first type of alteration.Temperature was probably close to 3000º b) A moderate to high salinity (15.3-24.5 wt% NaCl equiv.)heterogeneous (liquid + gas) CaCI2-NaCI-H20 fluid was in volved in the second alteration underconditions of Pfluid probably very close to hydrostatic. These alterations probably took place as discretehydrothermal events of different ages.
PB Sociedad Geológica de España
SN 0213-683X
YR 1997
FD 1997
LK https://hdl.handle.net/20.500.14352/56936
UL https://hdl.handle.net/20.500.14352/56936
LA spa
DS Docta Complutense
RD 16 may 2024