The P-T-t paths of high-grade gneisses, Kaoko Belt, Namibia: Constraints from mineral data, U-Pb allanite and monazite and Sm-Nd/Lu-Hf garnet ages and garnet ion probe data
Date
2014
Authors
Jung, S
Brandt, S
Nebel, Oliver
Hellebrand, E W G
Seth, B
Jung, C
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Elsevier
Abstract
The Damara Orogeny is a late Neoproterozoic to Cambrian (ca. 570-480Ma) intracratonic event that affected the Kaoko Belt, the inland branch of the Damara orogen and the Gariep Belt in Namibia and South Africa. This study focuses on the Pan-African evoluti
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Gondwana Research
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Journal article
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2037-12-31
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