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- W1978488084 endingPage "1412" @default.
- W1978488084 startingPage "1409" @default.
- W1978488084 abstract "Comparative geology suggests that the continents adjacent to northern, western, southern, and eastern Laurentia in the Late Proterozoic were Siberia, Australia-Antarctica, southern Africa, and Amazonia-Baltica, respectively. Late Proterozoic fragmentation of the supercontinent centered on Laurentia would then have been followed by rapid fan-like collapse of the (present) southern continents and eventual consolidation of East and West Gondwanaland. In this scenario, a pole of rotation near the Weddell Sea would explain the observed dominance of wrench tectonics in (present) east-west trending Pan-African mobile belts and subduction-accretion tectonics in north-south trending belts. In the process of fragmentation, rifts originating in the interior of the Late Proterozoic supercontinent became the external margins of Paleozoic Gondwanaland; exterior margins of the Late Proterozoic supercontinent became landlocked within the interior of Gondwanaland." @default.
- W1978488084 created "2016-06-24" @default.
- W1978488084 creator A5031766393 @default.
- W1978488084 date "1991-06-07" @default.
- W1978488084 modified "2023-10-10" @default.
- W1978488084 title "Did the Breakout of Laurentia Turn Gondwanaland Inside-Out?" @default.
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- W1978488084 doi "https://doi.org/10.1126/science.252.5011.1409" @default.
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