Early Cambrian magmatic arc flanked by an inverted Cambrian sedimentary basin in the Wilson Terrane of East Antarctica
The Ross Orogen, in East Antarctica, is linke d to Cambro-Ordovician subduction and terrane accretion processes along the paleo-Pacific active margin of Gondwana. Geological investigations within the partially exposed basement rocks of Northern Victoria Land (NVL) have revealed several major terrane...
| Main Authors: | , , |
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| Other Authors: | , |
| Format: | Conference Object |
| Language: | English |
| Published: |
2014
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| Subjects: | |
| Online Access: | http://hdl.handle.net/11567/856337 |