Abstract
Rb/Sr whole-rock ages from two suites of tholeiitic dykes establish a pre-3,600 Myr history for some granodioritic gneisses in the Limpopo Mobile Belt and identify two previously unrecognised magmatic events in the evolution of this region. This has important implications with regard to relationships between the Belt and the adjacent Rhodesian and Kaapvaal Cratons.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
