Structural evolution and tectonic context of the
The Ngubevu area lies in the westernmost extremity of the NTF inlier (Fig. 2, Fig. 3). It comprises that portion of the Mfongosi Group from the Ngubevu river to the Buffalo river, and incorporates three abandoned vein- and shear-zone hosted gold and base metal mines (de Klerk, 1995, Basson and Watkeys, 2000).
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