Tectono-metamorphic history of the re-worked, high-grade Maud Belt at central-Eastern H.U. Sverdrupfjella, Antarctica
The reworking of granulites by amphibolite- to granulite-facies metamorphism can complicate the interpretation of their geological history because the event that reached higher peak P-T conditions will either completely overprint earlier peak assemblages or prevent the formation of new 'peak�...
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| Format: | Dissertation |
| Language: | English |
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University of Cape Town
2016
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| Online Access: | http://hdl.handle.net/11427/16195 |