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Tectonic evolution of the Waldau Ridge structure and the Okahandja Lineament in part of the Central Damara Orogen, west of Okahandja, South West Africa
[page i missing] tonic igneous activity appears to have been in the form of aplite or quartzfelspar porphyry dykes (Gl). The Salem Granite Suite is the most widely represented granitic type and is to a large extent the ultra-metamorphic equivalent of part of the Kuiseb Formation. G2 granite is late...
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| Language: | English |
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Department of Geological Sciences
2024
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