. Lermontovskoe tungsten skarn deposit in central Sikhote‐Alin is concluded to have formed at 132 Ma in the Early Cretaceous, based on K‐Ar age data for muscovite concentrates from high‐grade scheelite ore and greisenized granite. Late Paleozoic limestone in Jurassic ‐ early Early Cretaceous accretionary complexes was replaced during hydrothermal activity related to the Lermontovskoe granodiorite stock of reduced type. The ores, characterized by Mo‐poor scheelite and Fe3+‐ poor mineral assemblages, indicate that this deposit is a reduced‐type tungsten skarn (Sato, 1980, 1982), in accordance with the reduced nature of the granodiorite stock. The Lermontovskoe deposit, the oldest mineralization so far known in the Sikhote‐Alin orogen, formed in the initial stage of Early Cretaceous felsic magmatism. The magmatism began shortly after the accretionary tectonics ceased, suggesting an abrupt change of subduction system. Style of the Early Cretaceous magmatism and mineralization is significantly different between central Sikhote‐Alin and Northeast Japan; reduced‐type and oxidized‐type, respectively. The different styles may reflect different tectonic environments; compressional and extensional, respectively. These two areas, which were closer together before the opening of the Japan Sea in the Miocene, may have been juxtaposed under a transpressional tectonic regime after the magmatism.