From 20 Ma till the end of the profile at 27 Ma, the mantle velocities follow a decreasing trend.
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Evolution of the Crustal and Upper Mantle Seismic Structure From 0-27 Ma in the Equatorial Atlantic Ocean at 2° 43'S.
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From 20 Ma till the end of the profile at 27 Ma, the mantle velocities follow a decreasing trend.