DACIAN BASIN - GeoEcoMar

1.5. Overview of the Dacian Basin cyclic development
clayey facies (littoral with very low sediment supply?) to sandy deltaic facies and
to fluvial sedimentation. This is observed on the right slope of the Luncavăţ River
(Cârstăneşti village, Vâlcea County), but the outcrops are discontinuous and partly
covered. A large scale coarsening upward prevailing tendency appears at Lunguleţu
geological section, followed by coarse-grained fluvial deposits (Fig. 1.9 A).
At the Bizdidel River section (Pucioasa, Dâmboviţa County) the Early Maeotian
part of the section is tectonically missing. The lower part of the Late Maeotian,
showing clear littoral (shore face and delta) features, is sharply overlaid by fluvial
deposits (Fig. 1.9 B).
FIGURE 1.9. Main features of the upper part of the Maeotian sedimentary sequence. A. Bistriţa
River, Lunguleţu village (Vâlcea County). B. Bizdidel River, Pucioasa (Dâmboviţa County).
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