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Geology and alteration-mineralization in the Gamigab area, north of the Brandberg / Felix C. Walraven

By: Material type: TextTextLanguage: English Series: Communications of the Geological Survey of South West Africa/Namibia, Volume 4, (1988) p. 83 - 88Publication details: Windhoek : Geological Survey of South West Africa/ Namibia, 1988,: Natal Witness Printing and Publishing Company (Pty) LtdDescription: 6 pages : fig.; 30 cmISSN:
  • 0256-1697
Subject(s): DDC classification:
  • PER 553 Communications of the Geological Survey of Namibia
Summary: In the Gamigab area, the mineralization was first investigated in 1953 by the South West Africa Company (SWA CO). The stratigraphy at the Gamigab Sn prospect consists of two mainly schistose units separated by a thick marble unit which have been correlated with the Orusewa Formation, the Karibib Formation and the Kuiseb Formation respectively. Four phases of folding affected the lithologies with the south-south-west trending F2 folds defining the main structures in the region
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In the Gamigab area, the mineralization was first investigated in 1953 by the South West Africa Company (SWA CO). The stratigraphy at the Gamigab Sn prospect consists of two mainly schistose units separated by a thick marble unit which have been correlated with the Orusewa Formation, the Karibib Formation and the Kuiseb Formation respectively. Four phases of folding affected the lithologies with the south-south-west trending F2 folds defining the main structures in the region

Geological Survey of South West Africa/ Namibia Serie

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