0000000000400329

AUTHOR

Clive Stowe

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Single zircon ages for two Archean banded migmatitic gneisses from central Zimbabwe

2004

We report new single zircon ages for two Archean banded gneisses from the Shangani Batholith in central Zimbabwe. The ages of ~2.77 and ~2.84 Ga do not support previous views that the area west of the current exposure of the Tokwe Segment was part of an early- to mid-Archean (>2.95 Ga) domain (Sebakwe Proto-craton). The data correspond to ~2.9 to 2.8 Ga dates for TTG granitoids of the Chingezi Suite. Members of this suite occur as intrusions within the south-central part of the Zimbabwe Craton and are associated with contemporaneous felsic volcanic rocks. On the basis of their age distribution, isotopic characteristics and outcrop pattern with respect to the Tokwe Segment, the formation of …

Volcanic rockCratongeographyIgneous rockgeography.geographical_feature_categoryFelsicBatholithArcheanGeochemistryGeologyGeologyZirconGneissSouth African Journal of Geology
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