Ratio of relative S to P velocity heterogeneity in the lower mantle
The parameter ν = ∂ ln υs/∂ ln υp, the ratio of relative S to P velocity heterogeneity, can be measured seismically and is important in determining the mineral physics of the deep mantle. However, seismic results are inconclusive because they have generally been based on P and S velocity models whic...
| Main Authors: | , |
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| Format: | Journal article |
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1996
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