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The Neoarchaean Tati granite-greenstone terrane occurs within the southwestern part of the Zimbabwe craton in NE Botswana. It comprises 10 intrusive bodies forming part of three distinct plutonic suites: (1) an earlier TTG suite dominated by tonalites, trondhjemites, Na-granites distributed into high-Al (Group 1) and low-Al (Group 2) TTG sub-suite rocks; (2) a Sanukitoid suite including gabbros and...
U-Pb SHRIMP single zircon crystallization ages were determined on representative samples of various granitoids exposed in the Vumba granite-greenstone terrain in NE Botswana. Based on structural and petrographic features, these granitoids were previously divided into five chronological groups: G1 (oldest) up to G5 (youngest). This chronology is not confirmed by U-Pb zircon dating, except for G5, which...
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