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and accumulation of thick rift-type sedimentary successions--has been recorded in South Australia, South China, Tarim, Kalahari, India, and the Arabian-Nubian Craton.
* Rifting progressed in the same cratons 800-750 Ma and spread into Laurentia and perhaps Siberia. India (including Madagascar) and the Congo-São Francisco Craton were either detached from Rodinia during this period or simply never were part of the supercontinent.
* As the central part of Rodinia reached the Equator around 750-700 Ma, a new pulse of magmatism and rifting

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