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Preliminary report on the stratigraphy of the Damara Sequence and the geology and geochemistry of Damaran granites in an area between Walvis Bay and Karibib / R. Brandt

By: Material type: TextTextLanguage: English Series: Communications of the Geological Survey of South West Africa/Namibia, Volume 1 (1985), p. 31 - 43Publication details: Windhoek : Geological Survey of South West Africa/ Namibia, 1985Description: 13 pages : tables, fig; 30 cmISSN:
  • 0256-1697
Subject(s): DDC classification:
  • PER 553 Communications of the Geological Survey of South West Africa/ Namibia
Summary: The rocks investigated in this study occur within the Central Zone of the Damara Orogen in the area between Walvis Bay and Karibib. In the course of the Damara Orogeny, the Damara succession as well as its Abbabis basement were intruded on a large scale by various magmas ranging from gabbroic to syenitic and granitic. It is the principal aim of the present study to unravel the relationships between the various intrusive rocks, to find out their protoliths and their position in the structural and metamorphic evolution of the Damara Orogen
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Uittrekesel in Afrikaans References

The rocks investigated in this study occur within the Central Zone of the Damara Orogen in the area between Walvis Bay and Karibib. In the course of the Damara Orogeny, the Damara succession as well as its Abbabis basement were intruded on a large scale by various magmas ranging from gabbroic to syenitic and granitic. It is the principal aim of the present study to unravel the relationships between the various intrusive rocks, to find out their protoliths and their position in the structural and metamorphic evolution of the Damara Orogen

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