Abstract
Fission-track dating was carried out for 18 tuff samples from the Pliocene strata in the Shinjo Basin, Yamagata Prefecture. After examination has been made to eliminate erroneous data by contamination of reworked zircon crystals, ages of the boundaries between the Nakawatari, Sakekawa, Yamuke and Motoaikai Formations are determined to be 4.3, 3.7 and 3 Ma, respectively.