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The sedimentology of the Zerrissene Turbidite System, Damara Orogen, Namibia / Roger Swart

By: Material type: TextTextLanguage: English Series: Geological Survey, Memoir No. 13, 1992Publication details: Windhoek : Geological Survey, 1992Description: viii, 54, III pages : tables, fig.; 30 cmISBN:
  • 0-86976-246- X
Subject(s): DDC classification:
  • PER 553a Geological Survey, Memoir
Summary: The late Proterozoic Damara Orogen of Namibia forms part of the Precambrian network of thermal, tectothermal and orogenic belts on the west of Africa and which is referred to as the Pan-African system of mobile belts. The orogen can be divided in two parts; a north-south trending coast-parallelarm which has a minimum width of 150 km, and a 400 km-wide northeasterly-orientated intracontinental arm. The northern junction between the two arms lies to the southwest of the Kamanjab Inlier. This study examines the sedimentological features of this zone and provides new data on the sedmientary history of the Damara Sequence
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The late Proterozoic Damara Orogen of Namibia forms part of the Precambrian network of thermal, tectothermal and orogenic belts on the west of Africa and which is referred to as the Pan-African system of mobile belts. The orogen can be divided in two parts; a north-south trending coast-parallelarm which has a minimum width of 150 km, and a 400 km-wide northeasterly-orientated intracontinental arm. The northern junction between the two arms lies to the southwest of the Kamanjab Inlier. This study examines the sedimentological features of this zone and provides new data on the sedmientary history of the Damara Sequence

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