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The structural evolution of an ancient accretionary prism in the Damara Belt, Namibia
The Southern Marginal Zone (SMZ) of the Damara Belt, exposed in the Gaub Canyon in central Namibia, consists of fourteen lithotectonic units of high strain amphiholite facies rock with pelagic, hemi-pelagic and clastic sedimentary protoliths. These rocks are intercalated With lenses of metabasite. R...
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| Language: | English |
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Department of Geological Sciences
2015
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