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...
| Main Authors: | , , , , |
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| Format: | Journal Article |
| Published: |
Elsevier Science BV
2008
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| Subjects: | |
| Online Access: | http://hdl.handle.net/20.500.11937/21860 |