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• W2000862340 abstract "Tomographic images of upper mantle velocity structure beneath an overlapping spreading center (OSC) on the East Pacific Rise indicate that this ridge axis discontinuity is underlain by a continuous region of low P-wave velocities. The anomalous structure can be explained by an approximately 16-kilometer-wide region of high temperatures and melt fractions of a few percent by volume. Our results show that OSCs are not necessarily associated with a discontinuity in melt supply and that both OSC limbs are supplied with melt from a mantle source located beneath the OSC. We conclude that tectonic segmentation of the ridge by OSCs is not the direct result of magmatic segmentation at mantle depths." @default.
• W2000862340 created "2016-06-24" @default.
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• W2000862340 date "2001-03-09" @default.
• W2000862340 modified "2023-10-06" @default.
• W2000862340 title "Continuous Mantle Melt Supply Beneath an Overlapping Spreading Center on the East Pacific Rise" @default.
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• W2000862340 doi "https://doi.org/10.1126/science.1057683" @default.
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