The geology and geochemistry of the Rooi Rand Dyke Swarm.
The Jurassic Rooi Rand dolerite dyke swarm was emplaced sub-parallel to the Lebombo Monocline during the initial stages of Gondwana breakup. The dykes extend northwards from the southern Lebombo region in northern KwaZulu-Natal, into central Swaziland, spanning a distance of approximately 200 kilome...
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| Language: | en |
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2012
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| Online Access: | http://hdl.handle.net/10413/4969 |