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Geochemical, Rb- Sr and U- Pb isotope studies of some acid volcanics from the Rehoboth Basement Inlier, Namibia : Report / G. F. U. Stoessel; U. R. F. Ziegler

By: Contributor(s): Material type: TextTextLanguage: English Series: Communications of the Geological Survey of Namibia, Volume 5, (1989) p. 77 - 83Publication details: Windhoek : Geological Survey of Namibia, 1989,: John MeinertDescription: 7 pages : tables, fig.; 30 cmISSN:
  • 0256-1697
Subject(s): DDC classification:
  • PER 553 Communications of the Geological Survey of Namibia
Summary: This report shows that all the analysed acid volcanics of the Rehoboth Basement Inlier are high-K rhyolites of mostly peraluminous nature. Acid volcanics occur throughout the Rehoboth Basement Inlier and are found as large extrusive masses of the Nückopf Formation as well as volcanic dykes crosscutting the Marienhof Formation, the Weener and Piksteel Intrusive Suites and the Gamsberg Granite Suite
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This report shows that all the analysed acid volcanics of the Rehoboth Basement Inlier are high-K rhyolites of mostly peraluminous nature. Acid volcanics occur throughout the Rehoboth Basement Inlier and are found as large extrusive masses of the Nückopf Formation as well as volcanic dykes crosscutting the Marienhof Formation, the Weener and Piksteel Intrusive Suites and the Gamsberg Granite Suite

A. Brückner Serie

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