Dome formation mechanisms in the southwestern Central Zone of the Damara Orogen, Namibia
No. 29, International Meeting of Young Researchers in Structural Geology and Tectonics (Part 1)
No. 29

Dome formation mechanisms in the southwestern Central Zone of the Damara Orogen, Namibia

International Meeting of Young Researchers in Structural Geology and Tectonics (Part 1)
  • L. Longridge
  • R. L. Gibson
  • J. A. Kinnaird
L. Longridge
R. L. Gibson
J. A. Kinnaird
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Longridge, L., Gibson, R. L., & Kinnaird, J. A. (2011). Dome formation mechanisms in the southwestern Central Zone of the Damara Orogen, Namibia. Trabajos De Geología, 29(29). Retrieved from https://reunido.uniovi.es/index.php/TDG/article/view/357
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Abstract

Mapping of the Palmenhorst and Ida Domes in the Central Zone of the Damara Orogen, Namibia, shows that Pan-African domal structures cored by Palaeoproterozoic basement gneiss have been formed by Type 2 fold interference between SSE-verging, recumbent folds and NE-trending, upright folds. Granite relationships indicate that the earlier SSE-verging event occurred at 520 Ma.
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