Fluid and deformation induced partial melting and melt escape in low-temperature granulite-facies metasediments, Damara Belt, Namibia.
Thesis (PhD (Earth Sciences))--University of Stellenbosch, 2009. === Fluid-present partial melting has generally been regarded a poor candidate for effecting crustal differentiation. In this study I report on anatectic metasediments from the Pan-African Damara Belt in Namibia that have undergone f...
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| Language: | en |
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Stellenbosch : University of Stellenbosch
2009
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| Online Access: | http://hdl.handle.net/10019.1/1226 |