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

Jung, S; Brandt, S; Nebel, Oliver; Hellebrand, E W G; Seth, B; Jung, C

doi:10.1016/j.gr.2013.05.017

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

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Jung, S; Brandt, S; Nebel, Oliver; Hellebrand, E W G; Seth, B; Jung, C

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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

Collections	ANU Research Publications
Date published:	2014
Type:	Journal article
URI:	http://hdl.handle.net/1885/77373
Source:	Gondwana Research
DOI:	10.1016/j.gr.2013.05.017

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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

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