Interaction of a mantle plume and a segmented mid-ocean ridge: Results from numerical modeling
Previous investigations have proposed that changes in lithospheric thickness across a transform fault, due to the juxtaposition of seafloor of different ages, can impede lateral dispersion of an on-ridge mantle plume. The application of this “transform damming” mechanism has been considered for seve...
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Veröffentlicht in: | Earth and planetary science letters 2014-04, Vol.392, p.113-120 |
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Sprache: | eng |
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