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Swiss Journal of Geosciences
Fig. 4 | Swiss Journal of Geosciences

Fig. 4

From: Structural and geochronological constraints from the Drina-Ivanjica thrust sheet (Western Serbia): implications for the Cretaceous–Paleogene tectonics of the Internal Dinarides

Fig. 4

Mesoscale D2 deformation structures. For outcrop locations see Fig. 2a. a Southwest-verging D2 reverse faults and related F2 folds in the Drina-Ivanjica Paleozoic (outcrop 006). b D2 thrust fault (top-SW tectonic transport) in the Albian-Campanian succession at outcrop 148B. c Top-NNE D2 reverse faults and related folds in the Southern Triassic unit (outcrop 067). d Geological cross-section at the boundary between the Drina-Ivanjica Paleozoic and the Southern Triassic unit (for section trace see Fig. 2a) showing the location of the observed structures at a smaller scale (bottom) and our interpretation of the observations. The vergence of folding and thrusting is top-NNE along the section

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