Fig. 17From: A tectono-stratigraphic record of an extensional basin: the Lower Jurassic Ab-Haji Formation of east-central IranPalaeogeography of east-central Iran (blocks and faults; modified from Zamani-Pedram (2011). A–C refer to Ravar–Abkuh (A), Zarand–Chenaruyeh (B), and Zarand–Eshkeli (C) and D–G refer to previously measured sections (Salehi et al. 2014a) of the Kuh-e-Rahdar (D), Simin-Sepahan (E), Parvadeh (F) and Kuh-e-Shisui (G) areas, respectively. Major strike-slip or reverse faults of central and eastern Iran: Kal Kalmard, Posht Posht-e-Badam, Raf Rafsanjan, Kb Kuh Banan, Bh Behabad, Ra Ravar, Lk Lakar Kuh. Rose diagrams represent palaeocurrents, n indicates the number of palaeocurrent measurements at each site. Circles indicate major citiesBack to article page