Inferring bedrock Cenozoic tectonics from ice surface pattern in the Dome C area, East Antarctica
East Antarctica is a Precambrian craton where the thickness of the crust is about 35-40 km. The main geological structures are buried by the extensive continental ice sheet apart from sparse outcrops along the perimeter of the continent. Present understanding of the tectonic evolution of East Antarc...
| Main Authors: | , |
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| Other Authors: | , |
| Format: | Other/Unknown Material |
| Language: | English Italian |
| Published: |
2004
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| Subjects: | |
| Online Access: | http://hdl.handle.net/11567/987286 |