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Fig. 3 | Swiss Journal of Geosciences

Fig. 3

From: Vertical-axis rotation in East Kopet Dagh, NE Iran, inferred from paleomagnetic data: oroclinal bending or complex local folding kinematics?

Fig. 3

Seismic section (a) and its interpretation (b) of a section cross-cutting the Kalat syncline in the west. See Fig. 2 for approximate location. Two minor north-verging thrusts in Jurassic strata root down into basement structures. In this and the subsequent figures: pJ pre-Jurassic, Jk Kashafrud Formation (Middle Jurassic), Jc Chaman Bid Formation (Upper Jurassic), Jm Mozduran Formation (Upper Jurassic); Shurijeh Formation (Lowermost Cretaceous), Kt Tirgan Formation (Barremian), Ksa Sarchashmeh Formation (Aptian), Ks Sanganeh Formation (Albian), Ka Aitamir Formation (Cenomanian), Kad Abderaz Formation (Upper Cretaceous), Kab Abtalkh Formation (Campanian), Kn Neyzar Formation (Campanian), Kk Kalat Formation (Campanian–Maastrichtian), PEp Pestehleigh Formation (Lower Paleocene), PEc Chehel Kaman Formation (Upper Paleocene)

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