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Kњига LXXII

Kњига LXXII

10 PLATON

10 PLATON TCHOUMATCHENCO, DRAGOMAN RABRENOVIĆ, VLADAN RADULOVIĆ, NENAD MALEŠEVIĆ & BARBARA RADULOVIĆ Fig. 4. A, Vratarnica Series, the “matrix” of the formation, near the road south of Vratarnica Village, Zaječar District; B, Vratarnica Series, olistolite of volcanogenous rock in the matrix, near the road south of Vratarnica Village, Zaječar District; C, Vratarnica Series, olistolite of coarse grained whitish limestone (analogous to the Crni Vrh Limestones of east Serbia or the Bulgarian Slivnitsa Formation) in the matrix, near the road south of Vratarnica Village, Zaječar District; D, Granitovo, Gradishteto Hill, syn-sedimentary fold in the upper part of the Gintsi Formation; E, Reverse fault in the upper part of the Gintsi Formation near Granitovo Village, Sokolov Venets Hill - in the upper part of the Gintsi Formation; F, reverse fault in the upper part of the Gintsi Formation, near the road Belogradchik–Railway Station Oreshets.

Trans-border (north-east Serbia/north-west Bulgaria) correlations of the Jurassic lithostratigraphic units 11 Fig. 5. A, Holotype section of the Sokolov Venets Zoogenous Marker, along the road Belogradchik–Railway Station Oreshets, general view and upper bed No 7; B, Holotype section of the Sokolov Venets Zoogenous Marker, along the road Belogradchik–Railway Station Oreshets, specimen from the lower bed No 6 – zoogenous breccia; C, Sokolov Venets Zoogenous Marker, view of the outcrop on the cliff by the road near Mitrovtsi Village, Montana District; D, Sokolov Venets Zoogenous Marker, view of the outcrop on the southern hill of the Gintski Venets (Cliff), near Gintsi Village, Sofia District, folded uppermost bed of the Bov (Polaten?) Formation; the sediments of the Sokolov Venets Zoogenous Marker fully fill the negative part of the ancient relief; in the right part of the photograph is seen the bed of the Polaten (Bov?) Formation overlaid by zoogenous breccia of the Sokolov Venets Zoogenous Marker; E, Desivitsa Member of the Polaten Formation in the Desivitsa Valley, near Prevala Village, Montana District; F, view of the Shugovitsa Slump; in the Shugovitsa River Valley, near Nikolovo Village, Montana District, the folds are in the Gintsi and the Glozhene Formations.

in Jurassic and Cretaceous Stratigraphy
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