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...
Published in: | Geology |
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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Geological Society of America Inc
2011
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Subjects: | |
Online Access: | https://hdl.handle.net/20.500.11937/15519 https://doi.org/10.1130/G31461.1 |