Rifting of the Kaapvaal Craton during the early Paleoproterozoic: Evidence from magmatism in the western Transvaal subbasin (South Africa)
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DOI: 10.1016/j.precamres.2020.105687
Abstract: Abstract The Neoarchean to Paleoproterozoic (ca. 2.65–2.06 Ga) Transvaal Supergroup of the Kaapvaal Craton is dominated by clastic and chemical sedimentary rocks, with few strata-bound igneous units. Two ca. 2.2 Ga igneous units in its upper part… read more here.
Keywords: paleoproterozoic; craton; igneous units; transvaal subbasin ... See more keywords