CONNECTING GEOLOGY AND GEOPHYSICS: THE GEODYNAMIC EVOLUTION OF DRONNING MAUD LAND FROM RODINIA TO GONDWANA
East Antarctica consists of a number of cratonic fragments that amalgamated along distinct orogenic belts in late Neoproterozoic to early Palaeozoic times. These mobile belts include the c. 640 to 500 Ma old East African-Antarctic Orogen (EAAO) and the Kuunga Orogen, which seem to converge in Dronni...
Main Authors: | , , , , , , , , , , , , , , |
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Format: | Conference Object |
Language: | unknown |
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Alfred Wegener Institute for Polar and Marine Research
2015
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Online Access: | https://epic.awi.de/38539/1/BzPM_0690_2015.pdf https://epic.awi.de/id/eprint/39617/ https://epic.awi.de/id/eprint/39617/1/Laeufer_etal_DGP2015.pdf https://hdl.handle.net/10013/epic.46790 https://hdl.handle.net/10013/epic.46790.d001 |