The geology and geochemistry of the Kadaweib complex, Red Sea Hills, Sudan

Formation of juvenile continental crust in the Arabian–Nubian shield: evidence from granitic rocks of the Nakasib suture, NE Sudan

“…Data are binned into 10-million-year 0.25% K 2 O intervals; means are reported for multiple analyses of individual plutons. Data sources are as follows: this study (marked with x); Bentor 1985;Beyth et al 1994;Bielski et al 1979;Dixon 1981a;Engel et al1980;Fullagar 1978;Greenberg 1981;Jarrar 1985;Jarrar et al 1983Jarrar et al , 1991Katz 1996;Klemenic and Poole 1984;Kröner et al 1990Kröner et al , 1991Kröner et al , 1994Schandelmeier et al 1994;Stein and Goldstein 1996;Stern and Kröner 1993;Stern and Dawoud 1991;Stern and Hedge 1985;Sturchio et al 1984 compositions, and only slightly different in terms of feldspar Pb isotopic compositions. With few exceptions, these isotopic characteristics are shared with neo-Proterozoic igneous rocks of eastern Egypt, Sinai, Israel, Jordan, and Saudi Arabia.…”