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- W2029942586 abstract "A large proportion of the African Crust yields Pan-African radiometric ages (650-450 Ma). The Pan-African domains form a network of mobile belts surrounding cratons which remained relatively stable, cool and undeformed. The crust in the Pan-African domains had a similar previous history to that in the cratons. There is no process of cratonization and no progressive increase in cratonic dimensions, only a progressive reduction in the area unaffected by successive deformations. Neither tectonic, structural, stratigraphic or palaeomagnetic data suggest large-scale plate motions. No convincing ophiolites or sutures have been recognized within the PanAfrican domains. In situ deformation rather than collision orogeny seems probable." @default.
- W2029942586 created "2016-06-24" @default.
- W2029942586 date "1976-01-22" @default.
- W2029942586 modified "2023-09-26" @default.
- W2029942586 title "A Discussion on global tectonics in Proterozoic times - Pan- African Structures" @default.
- W2029942586 doi "https://doi.org/10.1098/rsta.1976.0008" @default.
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