Subduction to post-collisional volcanism in the Northern Arabian-Nubian Shield: Genesis of Cryogenian/Ediacaran intermediate-felsic magmas and the lifespan of a Neoproterozoic mature island arc

• Published in: Precambrian research 2021-06, Vol.358, p.106148, Article 106148
• Main Authors: Maurice, Ayman E., Gharib, Moustafa E., Wilde, Simon A., Ali, Kamal A., Osman, Madiha S.M.
• Format: Article
• Language: English
• Subjects: Dokhan volcanics; Eastern Desert of Egypt; Felsites; Mature island arc; Neoproterozoic; Subduction
• ISSN: 0301-9268; 1872-7433
• DOI: 10.1016/j.precamres.2021.106148

•Dokhan andesite and dacite were erupted in a Neoproterozoic subduction setting.•The arc crust thickness (~32 km) is comparable to that of mature arcs.•Dokhan andesite and dacite are dated at ~ 660 Ma.•Post-Dokhan volcanics and felsites were formed in a post-collisional setting after ~ 600 Ma.•The magmatic arc lifespan was ~ 70 Ma. The Neoproterozoic intermediate-felsic volcanic rocks in the Wadi Ambagy area, Eastern Desert of Egypt, comprise three units: Dokhan intermediate-felsic volcanics, post-Dokhan felsic volcanics and felsites. The Dokhan lavas are generally porphyritic and composed of andesite and dacite with subordinate basalt, whereas the post-Dokhan felsic volcanics are represented by phyric and aphyric rhyolites. The medium-K calc-alkaline nature, LILE enrichment, Ta-Nb anomalies and LREE-enriched patterns of the Dokhan volcanic rocks are consistent with development in a subduction setting. Arc crustal thickness estimation using average (La/Yb)n is ~ 32 km, indicating that these rocks were generated in a Neoproterozoic island arc with thick crust. The subduction magmas were generated by hydrous mantle melting and they evolved by fractional crystallization. In contrast, the post-Dokhan felsic volcanics and felsites have medium- to high-K and shoshonitic affinities, respectively. They are highly silicic with weak to absent Ta-Nb anomalies and significant Nb, Zr, Hf and REE enrichment, which increases from the post-Dokhan felsic volcanics to the felsites. These geochemical features suggest generation in a post-collisional to within-plate tectonic setting by partial melting of mafic or intermediate arc crustal sources. SHRIMP U-Pb zircon dating indicates a crystallization age of ~ 660 Ma for the subduction-related Dokhan andesite and dacite, reflecting a magmatic arc lifespan longer than previously considered. The change of setting from subduction to post-collisional was accompanied by an increased role of crustal sources in the generation of the felsic magmas, resulting in differentiation of the accreted arc crust.