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Herein, correlations of the Jurassic sediments from NE Serbia with those of   NW Bulgaria are made. The following Jurassic palaeogeographic units: the   Eastern Getic, the Infra-Getic and the Moesian Platform are included in the   study. The East Getic was studied in the outcrops near Rgotina, where the   sedimentation started in the Hettangian and continued during the   Callovian-Late Jurassic and is represented by platform carbonates. The   Infra-Getic is documented by the sections of Dobra (Pesača) and the   allochtonous sediments near the Štubik. Very important for the Infra-Getic   are the Late Jurassic volcano-sedimentary deposits of the Vratarnica Series,   which crop out near Vratarnica Village. The Jurassic Moesian platform was   studied in the sections near D. Milanovac and Novo Korito (Serbia) and in   their prolongation in NW Bulgaria into the Gornobelotintsi palaeograben. Very   important are the correlation in the region of Vrška Čuka (Serbia) and   Vrashka Chuka (Bulgaria) - Rabisha Village (Magura Cave). A revision of the   Jurassic sediments on the Vidin palaeohorst, which were studied in the   Belogradchik palaeohorst, Gorno-Belotintsi palaeograben, Belimel palaeohorst   and the Mihaylovgrad palaeograben, is made. The sedimentation on the Vidin   palaeohorst started during different parts of the Middle Jurassic, and in the   Mihaylovgrad palaeograben during the Hettangian (Lower Jurassic) where the   sediments were deposited in relatively deeper water conditions. To south, the   relatively shallow water sediments deposited on the Jurassic Vratsa   palaeohorst on the southern board of the Mihaylovgrad palaeograben are   described

Trans-border (north-east Serbia/north-west Bulgaria) correlations of the Jurassic lithostratigraphic units