Zircon U-Pb-Hf evidence for subduction related crustal growth and reworking of Archaean crust within the Palaeoproterozoic Birimian terrane, West African Craton, SE Ghana
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文摘

Zircon U–Pb–Hf isotope data suggest mainly juvenile growth between 2.3 and 2.1 Ga.

Reworking of Archaean crust in southern Ghana is confined to between 2.141 and 2.126 Ga.

Combined isotope data suggest subduction related crustal growth.

Emplacement of 2.23 Ga granodiorite contradict suggested plume initiated subduction.

An evolutionary model is proposed.

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