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

• Published in: Precambrian Research
• Main Authors: Corvino, A., Boger, S., Henjes-Kunst, F., Wilson, C., Fitzsimons, Ian
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: Elsevier Science BV 2008
• Subjects: Rayner Belt; Prydz Belt; Palaeoproterozoic; East Antarctica; Zircon dating; Antarctic; Mawson Escarpment; Prince Charles Mountains; Rayner; The Antarctic; Antarc*; Antarctica
• Online Access: https://hdl.handle.net/20.500.11937/21860; https://doi.org/10.1016/j.precamres.2008.09.001

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...