Characteristic horizons designated by the author as «finplain horizons» have been described for the first time within the upper part of coarse molasse of Soviet Central Asia (Late Precambrian to Late Cenozoic in age); the horizons are characteristically different from the main part of the section both in thickness and lithology, and correspond to the stage of dynamic equilibrium which terminates (locally or in general) a phase of re-activation of the mountain topography development. Identification of the finplain horizons (and of other genetically similar formations within continental series) enlarges considerably both methodical and factological basis for paleogeomorphological analysis of orogens and on the other hand facilitates solving one of most complicated stratigraphic problems, that is unbiased stratification of coarse barren continental series.