Three-dimensional shear wave velocity structure in the Atlantic upper mantle
Oceanic lithosphere constitutes the upper boundary layer of the Earth’s convecting mantle. Its structure and evolution provide a vital window on the dynamics of the mantle and important clues to how the motions of Earth’s surface plates are coupled to convection in the mantle below. The three-dimens...
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| Language: | en_US |
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2016
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| Online Access: | https://hdl.handle.net/2144/17055 |