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  1. The 3 K/Ar ages derived from the hydrothermal alteration were 32 (30-34), 35 (34-36) and 37 (36-38) m.y., yielding an Oligocene age for the primary hydrothermal mineralization. Stepwise heating of the two samples from Pyrgi between 630 and 950 o C (91% of the 39Ar released in 6 steps) and 715 to 1000 o C (84% of the 39Ar released in 5 steps) respectively provided ages of 31.3-32.9 m.y. respectively, are in good agreement with the K/Ar age of 32 (30-34) m.y. From these data it can be concluded that the hydrothermal mineralization of Pyrgi (and probaby the whole Kato Nevrokopi region) took place at 32.5-33.0 m.y.