Fig. 15From: Vertical-axis rotation in East Kopet Dagh, NE Iran, inferred from paleomagnetic data: oroclinal bending or complex local folding kinematics?Satellite image of the Kalat syncline. Location is outlined by black box in Fig. 2. Red arrows: Paleomagnetic directions including value for declination for sites P01–P05. Red shade: Error of the paleomagnetic direction after Demarest (1983). Blue arrows: Direction perpendicular to the maximum axis of AMS ellipsoids for sites P01–P06 indicating main shortening (site P07 is statistically not relevant; see Table S1). Light blue arrows: AMS directions corrected for bedding tilt. Bottom left: Legend and overall mean paleomagnetic and AMS directions including valuesBack to article page