Aptian Stage is widespread in the Central North Bulgaria, while the Albian is established only in the northern regions. The Aptian sections are built up of sediments of the Trambes and Svištov Formations. It has been established that the Trâmbeš and Svištov Formation join laterally along the line Svištov-Tatari-Osilm. The concretion phosphorites and sandstones, with in the range of Albian, are
... [Show full abstract] here separated as Dekov Formations. The lithologic and ammonitic sequences in 9 sections are studied and described. Aptian Stage is represented by the Middle (Gargasian) and Upper (Clansayesian) Substages. The following ammonitic zones are separated and characterized: Cheloniceras (Epicheloniceras) martinioides Zone, C. (E.) subnodosocostatum Zone, Acanthohoplites nolani Zone, Hypacanthoplites jacobi Zone. Aptian is covered with a wash-out by Albian. The interruption of the sedimentation includes Late Aptian (partially), Early and Middle Albian (partially) Substages. Albian Stage is represented by the Middle (partially) and Upper Albian Substages. The following zones are established and characterized: Hoplites (Hoplites) dentatus Zone, Euhoplites loricatus Zone, Euhoplites lautus Zone, Mortoniceras (Pervinquieriа) inflatum Zone, Stoliczkaia dispar Zone. In some sections the separation of the first four zones is impossible due to the strong condensation in their basement. Albian is normally covered by Cenomanian. The boundary between them is traced by the disappearance of Stoliczkaia (Stoliczkaia), Mortoniceras and the appearance of Mantelliceras. Northwestwards an increase of the sandstones and mixed te rrigenous-carbonate rocks is observed in Aptian. An increase of the condensation and decrease of the thickness of the sediments to the south direction are established in Albian.