Tectonics of the north-western Gulf of Oman and the Arabian continental margin as indicated by magnetic data

Tectono-sedimentary framework of the Gachsaran Formation in the Zagros foreland basin

“…This fault divides not only the Persian Gulf from the Oman Sea at the eastern end of the Strait of Hormuz but also the eastern boundary of a widespread and intensive seismicity within the ZFTB ( Fig. 4; Glennie, 1996;Glennie et al, 1973;Hussieni, 1988;Khattab, 1994Khattab, , 1995. Beydoun et al (1992) suggested the Dibba fault as the eastern boundary of the Zagros foreland basin.…”