Iv. Kemkin, TECTONICS AND STRATIGRAPHY OF THE PEREKATNAYA-CHERNAYA INTERSTREAM AREA, SOUTHERN SIKHOTE-ALIN, Stratigraphy and geological correlation, 4(2), 1996, pp. 191-201
The geological structure of the Perekatnaya-Chernaya (Imbisha-Taukhe)
interstream area is represented by a complex combination of synsedimen
tary tectonic inclusions (allochthonous sheets of different origins an
d age ranges) embedded in a turbidite-olistostrome matrix. Three tecto
no-stratigraphic units of this type are distinguishable within the reg
ional section, which are amalgamated because of their accretion. Age c
onstraints for the matrix and tectonic inclusions are based on the dis
tribution of radiolarians.