Late Neoproterozoic 40° intraplate rotation within Australia allows for a tighter-fi tting and longer-lasting Rodinia
Previous paleomagnetic work has appeared to demand the breakup of southwest United States−East Antarctic (SWEAT) type Rodinia reconstructions before ca. 750 Ma, significantly earlier than the stratigraphic record of rift-drift transition between 715 Ma and 650 Ma. Here we reanalyze Australian paleom...
| Main Authors: | , |
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| Format: | Journal Article |
| Published: |
Geological Society of America Inc
2011
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| Online Access: | http://hdl.handle.net/20.500.11937/15519 |