Birimian crustal growth in the West African Craton : U-Pb, O and Lu-Hf isotope constraints from detrital zircon in major rivers

Summary, in English

Combined U-Pb, O and Lu-Hf isotope analyses of detrital zircon grains from five major rivers in Ghana are used to investigate the growth and evolution of the Birimian terrane of the West African Craton. The majority of the analysed zircon yields supra-chondritic ε_Hf values, suggesting derivation from primarily juvenile host magmas. Zircon grains from the Birim River in southwestern Ghana deviate from the generally juvenile trend, where the sub-chondritic ε_Hf but mantle-like δ¹⁸O of the 2.15 Ga population suggest reworking of ancient, but unweathered, meta-igneous crust. Hf-O isotope data from detrital zircons of the remaining rivers are consistent with sequential crust generation between ca. 2.2 and 2.1 Ga. Oxygen isotope data suggest that the contribution from Archaean sedimentary material to felsic magmas was below 30%, and in most cases below 10%. Zircon with strongly positive ε_Hf values and elevated δ¹⁸O indicate rapid reworking of juvenile crust within southern Ghana. An increase towards heavier oxygen isotope signatures over time suggests a maturing arc system with rapid recycling of juvenile supracrustal material during the evolution of the Birimian terrane.

• Author: Andreas Petersson; Anders Scherstén; Bara Kristinsdóttir; Anthony Kemp; Martin Whitehouse
• Department/s: Lithosphere and Biosphere Science
• Publishing year: 2018-02
• Language: English
• Pages: 259-271
• Publication/Series: Chemical Geology
• Volume: 479
• Links: http://dx.doi.org/10.1016/j.chemgeo.2018.01.021
• Document type: Journal article
• Publisher: Elsevier
• Topic: Geology; Geochemistry
• Keywords: Baoulé Mossi; Detrital zircon; Lu-Hf; Oxygen; U-Pb; West African Craton
• Status: Published
• ISBN/ISSN/Other: ISSN: 0009-2541