Superimposed tectonic events at 2450 Ma, 2100 Ma, 900 Ma and 500 Ma in the North Mawson Escarpment, Antarctic Prince Charles Mountains

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Superimposed tectonic events at 2450 Ma, 2100 Ma, 900 Ma and 500 Ma in the North Mawson Escarpment, Antarctic Prince Charles Mountains

The North Mawson Escarpment, in Antarctica's Prince Charles Mountains, forms part of a Palaeoproterozoic crustal complex which separates Archaean cratonic material to the south from Early Neoproterozoic and Early Palaeozoic metamorphic belts to the north. It consists of nappe-like masses of gre...

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Bibliographic Details
Main Authors:	Corvino, A., Boger, S., Henjes-Kunst, F., Wilson, C., Fitzsimons, Ian
Format:	Journal Article
Published:	Elsevier Science BV 2008
Subjects:	Rayner Belt Prydz Belt Palaeoproterozoic East Antarctica Zircon dating
Online Access:	http://hdl.handle.net/20.500.11937/21860

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