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

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

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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