RT Journal Article
T1 Datación por el método Sm-Nd del filón con F-Ba (Pb-Zn) de lamina San Eusebio (Sierra de Guadarrama, España)
A1 Galindo Francisco, Mª del Carmen
A1 Darbishyre, D.P.F.
A1 Tornos Arroyo, Fernando
A1 Casquet, César
AB Sm-Nd dating of F-Ba (Pb-Zn) veins enclosed in adamellites of the Spanish Central System suggests anage of 752±25 M.a. (Late jurassic) for this hydrothermal stage. This age supports an unconformity-relatedorigin for this style of mineralization and excludes any genetic relationship with a magmaticrelatedhydrothermal activity related to the enclosing granites. It is consistent with K-Ar and Rb-Srdating of other hydrothermal events in the Sierra de Guadarrama and strengthens the hypothesis thatthe late and posthercynian hydrothermal activity covers a long span of time.
PB Sociedad Geológica de España
SN 0213-683X
YR 1993
FD 1993
LK https://hdl.handle.net/20.500.14352/56935
UL https://hdl.handle.net/20.500.14352/56935
LA spa
DS Docta Complutense
RD 1 may 2024