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...

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Bibliographic Details
Main Authors: Jacobs, Jeffrey Bruce, Klemd, R, Fanning, Christopher, Bauer, Wolfgang, Colombo, Fabrizio
Other Authors: M. Yoshida, B.F. Windley, S. Dasgupta
Format: Book Part
Language:unknown
Published: Geological Society of London 2015
Subjects:
Online Access:http://hdl.handle.net/1885/86037