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- W1580163000 abstract "Published geological and geophysical data are reviewed. The Walvis Ridge is a complex linear feature made up of three parts of unequal lengths and differing basement morphologies: an eastern sector composed of rugged, subparallel basement ridges; a low-lying central sector with subdued basement morphology; and a western sector consisting of seamounts and guyots (including Tristan da Cunha and Gough islands). Rock samples and geophysical data suggest that the Ridge is composed of alkali basalt which becomes progressively older eastwards. Gravity data indicate that at least parts of the ridge are in local isostatic equilibrium. A mantle plume mechanism of formation is rejected in favour of a centre of abnormally high volcanic activity on the spreading ridge axis. The location of this centre, whose relative movement has been southwards, is determined by fracture zones crossing the spreading ridge axis." @default.
- W1580163000 created "2016-06-24" @default.
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- W1580163000 date "2013-03-21" @default.
- W1580163000 modified "2023-10-14" @default.
- W1580163000 title "The Walvis Ridge : A Review" @default.
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- W1580163000 doi "https://doi.org/10.1029/sp005p0160" @default.
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