High-temperature metamorphism in the western Namaqua-Natal Metamorphic Province (South Africa): implications for low-pressure granulite terranes
The interpretation of pressure (P)-temperature (T)-time (t) data is key to reconstruct the geologic evolution of ancient exhumed orogens. Of these, temperature is regarded as proxy for the heat energy available during orogenic metamorphism. Heat - the ultimate driving force of metamorphism - is cons...
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| Format: | Doctoral Thesis |
| Language: | en |
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University of Cape Town
2019
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| Online Access: | http://hdl.handle.net/11427/30410 |