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The Damara mobile belt in the south-Western Kaokoveld
After the establishment of the N-S Andib-Ganamub trough, the ubiquitous Lower Nosib subarkose was succeeded in the west by the Upper Nosib greywacke which indicates that orthogeosynclinal subsidence was already active in pre-Damara times. A pulse of NNE folding (F₁N) concluded this sedinentary cycle...
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| Language: | English English |
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Department of Geological Sciences
2017
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