New high spatial resolution secondary ion mass spectrometry (SIMS) zircon dating from the Dire Dawa Precambrian basement yields crystallization ages at c. 790 Ma and 600 - 560 Ma. Two of the youngest samples are pervasively deformed, indicating that orogenesis continued until c. 560 Ma. SIMS delta O-18(zrn) shows bimodality, with the oldest sample (c. 790 Ma) and inherited zircons of that age in the younger samples having values of 7.8 - 9.6%, whereas the Ediacaran samples have delta O-18(zrn) values of 4.9 - 7.2%. These delta O-18(zrn) ratios are higher than mantle values and indicate a supracrustal input to the source of the Dire Dawa granitoids. All samples have unradiogenic epsilon(Nd)(t) values of -10.3 to -5.8 and Nd model ages of 1.72-1.42 Ga. These attributes suggest that the Dire Dawa granitoids were mostly derived from reworking of long-lived crustal sources. The occurrence of c. 580 - 550 Ma orogenesis in both the Dire Dawa basement and the juvenile Western Ethiopian Shield and the confinement of c. 630 Ma metamorphism to only the latter indicate that these two lithospheric blocks of contrasting isotopic compositions amalgamated at c. 580 - 550 Ma. This suggests that the Mozambique Ocean, which separated these two lithospheric blocks, was completely consumed during the late Ediacaran to early Cambrian.

High-spatial-resolution secondary-ion mass spectrometry (SIMS) U-Pb zircon ages, whole-rock Nd isotopic and geochemical data are reported for granites and granitic gneisses from a traverse across the Abas terrane, Yemen, a part of the Precambrian basement of southern Arabian Peninsula. SIMS U-Pb dating identifies two magmatic episodes, the first at c. 790-725 Ma represented by granitic gneisses, the second clearly post-tectonic at c. 625-590 Ma. The oldest sample in the post-tectonic group is slightly deformed while younger samples are undeformed indicating that penetrative deformation ceased at c. 625 Ma in the Abas region. Whole-rock(Nd)(t) values between -11 and +0.8, Nd model ages of 1.70-1.13 Ga indicate a significant contribution of evolved continental material in the genesis of the Abas granitoids, unlike most of the juvenile Arabian-Nubian Shield (ANS), although there are few inherited zircons. Secular variation in epsilon(Nd)(t)reflects a change in magma source with increasing juvenile magma and diminishing crustal input during post-tectonic (625-590 Ma) magmatism. The combination of subduction zone chemistry, absence of older rocks, paucity of inherited zircons, evolved Nd isotopic signatures and the I-type characteristics of the samples suggest that assimilation occurred at depth.

Secondary ion mass spectrometry (SIMS) U-Pb zircon dating of plutonic rocks from the southernmost Arabian Shield identifies the earliest diorite–trondhjemite batholith emplacement at ca. 810 Ma and a second phase of plutonism of similar composition at ca. 685–665 Ma. A major shift in plutonic composition is marked by the emplacement of gneiss domes dated at ca. 770 Ma. Trace element ratios such as high Ba/La, Ba/Nb and Pb/Ce suggest a sub-arc mantle metasomatized by slab-derived fluids. The Th/Ce ratios are also higher than global subducting sediment (GLOSS) and suggesting an incompatible element-enriched mantle source. The distribution in Ta/Nb of the arc related samples beyond the field of mantle-derived magmas suggests a continental influence. From these geochemical characteristics, we conclude that a subducted slab/sediment component, rather than an OIB-like source, is likely. A slab component for the island-arc samples is also corroborated by their typical adakite-like geochemical traits, such as ≥ 60 wt.% SiO₂, high Mg# (34–77), high Sr (450–2240 ppm), low HREE and HFSE (0.2–1.1 ppm Yb and 2.6–15.6 ppm Y) and consequently elevated Sr/Y of 117–285, high Ni and Cr contents and negligible Eu-anomalies. All samples gave ε_Nd(t) values of +3.9 to +6.9, overlapping with the western arc terranes of the Arabian Shield, indicating the juvenile nature of the crust in the southernmost Arabian Shield. However, there is a subtle secular variation in ε_Nd(t) with the younger post–tectonic samples being slightly less juvenile. This suggests that the younger plutons were contaminated by minor evolved material.

The juvenile Neoproterozoic basement of the Arabian Shield is overlain with angular unconformity by a voluminous Cambro-Ordovician cover sequence known as the Saq Formation and Wajid Group. Provenance studies of this vast siliciclastic cover over the Saudi Arabian part of the Arabian-Nubian Shield (ANS) have to date been based solely on U-Pb zircon data and heavy minerals. We present the first combined in-situ U-Pb, δ¹⁸O and Lu-Hf isotopic data for detrital zircon from the Saq and Wajid units exposed along the northeastern margin and southern part of the Arabian Shield. U-Pb age spectra reveal prominent age peaks at ca. 0.8–0.55 Ga and 1.1–0.9 Ga with subordinate peaks at ca. 2.2–1.7 Ga and 2.7–2.5 Ga. The δ¹⁸O secular variation mirrors global compilations with Archaean zircon defining a restricted δ¹⁸O range of ca. 4.0–8.0 ‰ and younger zircon showing wide variation in δ¹⁸O up to ca. 14 ‰. The ca. 0.8–0.55 Ga age peak has the largest variation in ε_Hf(t) with about half of all these Neoproterozoic zircon grains being juvenile (ε_Hf(t) > 5), which are interpreted to be sourced from the juvenile terranes of the ANS. Neoproterozoic zircon with evolved ε_Hf(t) signatures require a more distal source beyond the ANS. As extensive ca. 1.1–0.9 Ga crust is lacking in the vicinity of the ANS, the ca. 1.1–0.9 Ga age peak is interpreted to be derived from either contemporaneous orogenic belts in Central Africa or recycled from older sedimentary rocks containing these age components. Extreme variations in δ¹⁸O of post–Archaean zircon, together with the evolved ε_Hf(t), indicate crustal thickening and increased incorporation of supracrustal material associated with collisional orogenesis. The remarkable similarities in age spectra and isotopic compositions of the Saq Formation and Wajid Group sandstones with those from other regions in northern Gondwana indicate a continental–scale homogenization and dispersion process.