@article{10272/13935,
year = {1994},
url = {http://hdl.handle.net/10272/13935},
abstract = {Two calcalkaline granite porphyries, an E-W and a N-S trending one, and three monzonitic dykes striking NE-SW, have been dated. For the first dyke a whole rock Rb-Sr isochrone age of296±3 Ma, i.e. Upper Carboniferous, is obtained. However, the second dyke provides only a regression age of 314±31 Ma. Whole rock K-Ar ages of the monzonitic dykes are 245±7, i.e. Lower-Middle Triassic, for two of them, and 220±5 for the third. The first age rises doubts about the up-to-the-present alleged posteriority of the E-W dykes relative to the large granitic plutonism in the area. The second is geologically reasonable within the limits of error only, as N-S dykes must be younger than the Cabeza Mediana pluton, which is 291+6 Ma old, and older than the hydrothermal episyenitic event dated at 274 ± 6 Ma. For the monzonitic dykes the age of 245 ± 7 Ma is taken as representative of the injection episode, whilst the second age probably results from superimposed alteration. This alkaline episode can be correlated with the opening of the Iberian trough},
publisher = {Sociedad Geológica de España},
title = {Cronología Rb-Sr y K-Ar de diques de la Sierra de Guadarrama (Sistema Central Español)},
title = {Rb-Sr and K-Ar chronology of dykes from the Sierra de Guadarrama (Spanish Central System)},
author = {Galindo, Carmen and Huertas, María José and Casquet Martín, César},
}