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Swiss Journal of Geosciences
Fig. 5 | Swiss Journal of Geosciences

Fig. 5

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

Fig. 5

Stereographic projections of fault-slip data collected in the study area. The locations of measurements are indicated by the number in the top right corner of the boxes. The data are grouped according to the distinguished deformation phases (D3 strike-slip faulting, D4 orogen-perpendicular and orogen-parallel extension). ANG, RUP are the quality indices of the paleostress calculations (for details see Angelier 1984). ANG: angular difference between the measured striae and the “ideal” striae calculated on the basis of the determined tensor. RUP: difference between the calculated shear stress vector of a particular fault and the absolute value of the vector that is requisite to produce slip on that plane. Phi (Φ) is the ration of stress axes (σ2 − σ3)/(σ1 − σ2)

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