The Mushandike granite: further evidence for 3.4 Ga magmatism in the Zimbabwe craton
The conflict between independently published ages for the Mushandike Granite, Zimbabwe (2.92 ± 0.17 Ga and 3.45 ± 0.13 Ga) has been resolved in favour of the older age by SHRIMP U-Pb analyses of zircon. Two samples yield indistinguishable estimates of 3
|Collections||ANU Research Publications|
Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.