Time scales and mechanisms of growth of active margins of Gondwana: A model based on detrital zircon ages from the Neoproterozoic to Cambrian Blovice accretionary complex, Bohemian Massif
Cadomian accretion in the Blovice accretionary complex lasted till ca. 527 Ma. Sedimentation in younger forearc basins continued at least till 499 Ma. Cadomian evolution of this complex is similar with that of the Ossa Morena.