Abstract
Fission-track dating was carried out on zircon crystals in a pumice obtained from a tuffbed in the Katsurane Facies in the Tentokuji Formation at Hanekawa, Akita City. As a result, the first reliable radiometric age of 4.4±0.6 Ma (2σ) was obtained for the tuffbed. The result supports the correlation between the Katsurane Fades distributed on surface outcrops and that distributed in offshore sub-surface wells.