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Fluid and deformation induced partial melting and melt escape in low-temperature granulite-facies metasediments, Damara Belt, Namibia.
(Stellenbosch : University of Stellenbosch, 2009-03)
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 ...