U-Pb zircon age for the Umkondo dolerites, eastern Zimbabwe: 1.1 Ga large igneous province in southern Africa East Antarctica and possible Rodinia correlations
Re. Hanson et al., U-Pb zircon age for the Umkondo dolerites, eastern Zimbabwe: 1.1 Ga large igneous province in southern Africa East Antarctica and possible Rodinia correlations, GEOLOGY, 26(12), 1998, pp. 1143-1146
We report a U-Pb zircon age of 1105 +/- 2 Ma for the extensive Umkondo dole
rites in eastern Zimbabwe, which are part of a large igneous province that
can be traced over much of southern Africa and originally contiguous parts
of East Antarctica. Other members of the province include widespread tholei
itic intrusions in Botswana and South Africa, bimodal volcanic rocks in Bot
swana and Namibia, and dolerites and flood basalts in Dronning Maud Land, A
ntarctica. Available data indicate that substantial parts of the province w
ere emplaced in a restricted interval at ca. 1.1 Ga and originated from a l
arge-scale mantle thermal anomaly inboard of a coeval continental-margin or
ogen, Striking similarities in age and tectonic setting between the Umkondo
igneous province and widespread 1.1 Ga within-plate magmatism in Laurentia
are consistent with reconstructions of the early Neoproterozoic Rodinia su
percontinent that place southern Africa and Dronning Maud Land off the sout
hern tip of Laurentia.