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- W2032027424 abstract "Differentiation of crust and mantle components during ascent between steadily diverging plates follows a simple law independent of the shape of the conduit and the spreading velocity under fairly general conditions. If the upward velocities of crust and mantle components are of the same order of magnitude, the rising column contains two to four times as much crustal material as the lithosphere that it creates. This paradox, which is unique to a spreading system, can substantially influence estimates of the gravitational driving pressure for the ascent of new material beneath an oceanic ridge. The model also implies that the lithosphere is enriched in crustal component relative to its source in the asthenosphere by the ratio of the upward velocities of the crust and mantle components." @default.
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- W2032027424 date "1973-02-10" @default.
- W2032027424 modified "2023-10-11" @default.
- W2032027424 title "Differentiation and the gravitational driving force for material rising at an oceanic ridge" @default.
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- W2032027424 doi "https://doi.org/10.1029/jb078i005p00825" @default.
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