Extensional collapse of the late Neoproterozoic-early Palaeozoic East African-Antarctic Orogen in central Dronning Maud Land, East Antarctica
The East African-Antarctica Orogen resulted from the continent-continent collision of East and West Gondwana, or parts thereof, during the Pan-African event at c. 650-510 Ma. The collision overprinted large areas of older, mainly Mesoproterozoic, crust up to granulite facies grade in East Antarctica...
Published in: | Geological Society, London, Special Publications |
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Main Authors: | , , , , |
Format: | Book Part |
Language: | unknown |
Published: |
Geological Society of London
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Subjects: | |
Online Access: | http://hdl.handle.net/1885/86037 https://doi.org/10.1144/GSL.SP.2003.206.01.14 |