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- W2045295532 abstract "A combined analysis of SKS , SKKS and P 660 s seismic phases detected in the records of BCAO/BNG seismic station in central Africa reveals that the waveform and amplitude of the T component of P660s deviate significantly from those predicted from the observations of shear wave splitting in SKS and SKKS . The inverse problem is investigated by using the anisotropic Thomson‐Haskell code and a genetic algorithm. The discrepancy between SKS/SKKS and P 660 S can be explained by P‐SH conversion at the boundaries of a weakly anisotropic layer 30–40 km thick lying atop 660 km discontinuity beneath BCAO/BNG. This anisotropy is probably induced by horizontal flow at the bottom of the upper mantle, in the transition zone." @default.
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- W2045295532 date "1998-06-01" @default.
- W2045295532 modified "2023-10-18" @default.
- W2045295532 title "Seismic evidence of flow at the base of the upper mantle" @default.
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- W2045295532 doi "https://doi.org/10.1029/98gl01418" @default.
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