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Metamorphism of pelites in the upper Black Nossob River area of the eastern Damara Orogen / K. W. Kasch

By: Material type: TextTextLanguage: English Series: Communications of the Geological Survey of South West Africa/Namibia, Volume 3, (1987) p. 63 - 81Publication details: Windhoek : Geological Survey of South West Africa/ Namibia, 1987Description: 19 pages : tables, fig.; 30 cmISSN:
  • 0256-1697
Subject(s): DDC classification:
  • PER 553 Communications of the Geological Survey of Namibia
Summary: The upper Black Nossob River area is located in the eastern part of the Damara Orogen between Okahandja and Steinhausen. The aim of this investigation was to map metamorphic zones in the upper Black Nossob River area and to study the regional variation in temperature and pressure by quantitative geothermometry and geobarometry. Furthermore an attempt has been made to compare and contrast the tectonothermal evolution of the major tectonic units of this area
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The upper Black Nossob River area is located in the eastern part of the Damara Orogen between Okahandja and Steinhausen. The aim of this investigation was to map metamorphic zones in the upper Black Nossob River area and to study the regional variation in temperature and pressure by quantitative geothermometry and geobarometry. Furthermore an attempt has been made to compare and contrast the tectonothermal evolution of the major tectonic units of this area

Geological Survey of South West Africa/ Namibia Serie

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