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- W2050186146 abstract "A series of seismic refraction profiles has been shot between Kenya and the Seychelles Bank and in the neighbourhood of the Bank itself. Thick sediments have been observed for 300 to 400 km from the African coast. Near Kenya, great thicknesses of material of about 4.8 km/s velocity match closely the 9 to 10 km of Karroo beds expected on the coast at Lamu. The Mohorovicic discontinuity has been traced from 100 km off the African coast to the Seychelles Bank. West of the Bank the mantle is unusually shallow, rising to only 8.5 km below the surface, and the 6.8 km/s crustal layer unusually thin or absent. The absence of a gravity anomaly associated with this very shallow mantle raises a problem which has yet to be resolved." @default.
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- W2050186146 date "1966-04-07" @default.
- W2050186146 modified "2023-09-26" @default.
- W2050186146 title "A discussion concerning the floor of the northwest Indian Ocean - Crustal structure between Kenya and the Seychelles" @default.
- W2050186146 cites W1967784774 @default.
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- W2050186146 doi "https://doi.org/10.1098/rsta.1966.0010" @default.
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