Abstract
Two granitoid samples from Vladivostok of southern part of the Voznesenka Belt yield 427.0 ± 3.1 Ma and 254 ± 3.4 Ma. Five granitoid samples from the Maizuru Belt yield 259.0 ± 3.0 Ma, 291.6 ± 4.3 Ma, 294.0 ± 4.5 Ma, 279.7 ± 2.4 Ma and 441.9 ± 2.8 Ma. The uncertainties in the ages are 95 % confidence interval (1.96 σ). Reffering to the coexistence of Triassic sequence and Silurian and Permo-Triassic granitoids, it seems that there are strong relations between the Maizuru Belt and southern part of the Voznesenka Belt.