Geological fluid inclusion and geochronological studies carried in work show that the Sierra del Guadarrama has an important hydrothermal activity that spans, at least, during 200 M.a affter the intrusion of the hercynian granitoids. Only the earliest hydrothermal events are related to these granitoids, while the majority of the hydrothermal alterations are related to regional hydrothermal convective systems. The hydrothermal events are superimposed in time and space due to reactivation of faults.
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