Hf isotopic composition of single zircons from Neoproterozoic arc volcanics and post-collision granites, Eastern Desert of Egypt: Implications for crustal growth and recycling in the Arabian-Nubian Shield

• New Hf-isotopic analyses of zircon from the Eastern Desert of Egypt.
• Hf-TDM ages for post-collisional granites range between 0.81 and 1.3 Ga.
• Post-collisional granite results indicate evolving juvenile crust.
• Hf-TDM ages for arc-metavolcanic rocks range between 0.78 and 3.8 Ga.
• Arc-metavolcanicHf results indicate involvement of pre-Neoproterozoic material.

Zircon Hf isotopic compositions for Neoproterozoic igneous rocks in the Central Eastern Desert of Egypt are presented and interpreted. The Humr Akarim (633 ± 7 and 603 ± 9 Ma)–Humrat Mukbid (625 ± 8 and 619 ± 8 Ma) plutons are Early Ediacaran post-collsional subsolvus granites. Their zircon ages range from 0.57 to 0.71 Ga, with high positive ɛHf(T) values of +4.0 to +11.9. Hf model ages (Hf-TDMc) of 0.81–1.3 Ga, are close to the U–Pb crystallization ages. These isotopic characteristics, along with published whole-rock Nd isotopic data, indicate that the protoliths were juvenile. The Wadi Kareim and Wadi El-Dabbah metavolcano-sedimentary rocks are Cryogenian (∼750 Ma) arc-related metabasalts, meta-andesites and meta-tuffs. Their U–Pb zircon age populations range between 0.7–0.9, 0.9–1.5 Ga and 2.0–3.0 Ga. The youngest group represents magmatic zircons in the metavolcanics or reworked Neoproterozoic rocks in the metasediments. The 0.9–1.5 Ga and 2.0–3.0 Ga age groups are similar to those in pre-Neoproterozoic rocks that surround the Arabian-Nubian Shield and represent inherited or older detrital grains. The highly variable ɛHf(T) values (+23.5 to −35.0) and Hf-TDMc ages (0.78–3.8 Ga) of Neoproterozoic zircons indicate that at least some of these magmas interacted with a pre-Neoproterozoic crustal source.

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