The African continent is unique in that it has escaped widespread
orogenic activity after the Pan African orogenic event. Therefore,
the African Plate provides the world's best example of the
relationship between extensional magmatism and structural setting.
This first complete and up-to-date review, written by leading
scientists, discusses the evolutionary model and offers a new and
reliable basis for scientists working on plate tectonics and
extensional areas in other continents.
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