In recent years, an independent complex of dikes of diorite porphyrites, granite porphyries, and granosyenite porphyries of Cretaceous age, confined to the zone of intense Mesozoic activation of the Precambrian platform, has been identified in the central part of the Stanova folded area. The dikes were described by E. P. Gurova and E. P. Gurova and E. P. Gurov, who, unfortunately, did not take into account the works of the FESU, described in this article.