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A structural and geochemical traverse across the NW outcrop of the Colenso Fault Zone, Saldanha, South Africa
The Colenso Fault Zone marks the boundary between the Tygerberg and Swartland Terranes in the Pan-African Saldania Orogenic Belt. The fault zone comprises several discrete shear discontinuities that in places cross-cut relatively undeformed granites of the Cape Granite Suite. It is NW-SE striking, ~...
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| Language: | English |
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Department of Geological Sciences
2016
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