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Fitch, Basement faultln8 and focal depths of the larger earthquakes in the Zagros mountains (Iran), Geophys. J. Roy. astr. Soc.~ 64, 561-586, 1981. Jakson, J.A., T.J. Fitch, and D.P. MeKenzle, Actlve tectonics and the evolution of the Zagros fold belt, Geol, SOc. Lond., sp. Pub. 9__, 1981. ACTIVE FAULTING AND TECTONICS OF IRAN 65
Page 1 and 2: Reprinted from Zagros ¯ Hindu Kush
Page 3 and 4: Inset left: Dlstrlbutlon ofeplcentr
Page 5 and 6: Araxlan-Azarbaijan zone of Caledoni
Page 7 and 8: GULF OF OMAN Fig. ~. Fault Hap of I
Page 9 and 10: 2. Segments of the High Zagros deep
Page 11 and 12: TABLE I. Cont. F~_U~LT # ~L~ME FT F
Page 13 and 14: 11Ambraseys 1974 24 A=braseys 1963
Page 15 and 16: ~ U.PRECAMBRIAN HORMOZ SALT TECTONI
Page 17 and 18: TABLE II - Seismic trends (buried h
Page 19 and 20: Indicating that the reglon ls asets
Page 21 and 22: |Taba s J J Khaf Sabzevar Kuh Banan
Page 23 and 24: CASPIAN SEA 0 200 km 1979 38’ AFG
Page 25 and 26: CASPIAN SEA GULF OF OMAN Fig. 12. E
Page 27 and 28: Dominance of 170 My or 210 My of An
Page 29 and 30: 1977, Sykes 1978] and the deformati
Page 31: the fact that the cruat consists of
Page 35 and 36: Nabavi, M.S., Selsmicity o£ Iran,
Page 37: Wowroo zi, Seismological and geolog

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