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- W2341492403 abstract "Areas of volcanic over-production within the oceanic crust, such as linear chains of oceanic islands and seamounts, have traditionally been explained in terms of mantle plumes. For the South Atlantic Ocean, however, it appears that processes operating at the mid-ocean ridge may provide the dominant control. A model is proposed based on satellite-derived free air gravity and Global Positioning System (GPS) plate motion data, combined with extensive knowledge of the tectonic processes that have operated in the adjacent continents of Africa and South America. During the Central and South Atlantic opening, differential motion between plate segments was principally absorbed within..." @default.
- W2341492403 created "2016-06-24" @default.
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- W2341492403 date "2005-01-01" @default.
- W2341492403 modified "2023-10-06" @default.
- W2341492403 title "Plate tectonic processes in the South Atlantic Ocean: Do we need deep mantle plumes?" @default.
- W2341492403 doi "https://doi.org/10.1130/0-8137-2388-4.537" @default.
- W2341492403 hasPublicationYear "2005" @default.
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