“…Babalola (1999) and Hussain et al (2004) also concluded that most likely provenances of the lower part of the Wajid Sandstone are dominantly the acid igneous and gneissic metamorphic rocks of the Neoproterozoic Afif, Abas, Al-Bayda, Al-Mahfid, and Al-Mukalla terranes (Windley et al (1996) to the south. Heavy mineral data of the Cambrian section of southern Israel and Jordan (Weissbrod and Nachmias, 1986;Amireh, 1991) are rich in stable heavy mineral assemblage of zircon-rutile-tourmaline suggesting long-distance (over 1000 km, Garfunkel, 1999) transportation.…”